With the continuous expansion of oil and gas exploration into ultra-deep and ancient strata in the three major marine cratonic basins, challenges such as unclear favorable exploration zones have emerged. Therefore it is imperative to deepen research on depositional models for critical geological periods. Based on the summary of the Neoproterozoic-Paleozoic tectonic-sedimentary differential evolution characteristics of the three major basins, this paper analyzes the controlling effects of tectonic differentiation on sedimentary evolution. It is pointed out that the three ancient marine cratonic basins exhibit a tectonic differentiation pattern of "rift-depression-uplift", driving carbonate platforms undergoing an evolutionary cycle of "isolated platform-ramp-rimmed platform", and the formation and evolution of rifts control the sedimentary differentiation of platforms and the similarity of the vertical sourced-reservoer-cap assemblages. Four new models of carbonate sedimentation were established: "multi-type platform margins" and "double shoals" ramp models, carbonate-gypsum/salt symbiotic system model, fault terrace platform margin model of Dengying Formation in Sichuan Basin, and continuously expanding platform margin sedimentary model of Cambrian in Tarim Basin. The "multi-type platform margins" and "double shoals" ramp model reveal that the continental margin and rift margin, depression margin, paleo-uplift of inner ramp and lagoon periphery are favorable mound-shoal development areas. The carbonate-gypsum/salt symbiotic system model reveals that the margin of the paleo-uplift during transgression period is a favorable shoal development area. The fault terrace platform margin sedimentary model indicates that multiple syndepositional fault systems control the formation of step-like platform margins of the 2nd member of Dengying Formation in Sichuan Basin, with thick mound-shoal complexes developed on high fault blocks. The continuous extension platform margin sedimentary model reveals that the Cambrian platform margin belt of Lunnan-Gucheng area in Tarim Basin has undergone the evolution of mud-rich ramp→low-angle progradational ramp/weakly rimmed platform→vertically aggrading platform→laterally prograding rimmed platform. The new understanding of carbonate sedimentary models confirms that the mound-shoal belts around the paleo-rift of the three ancient marine craton basins are still important areas for increasing oil and gas reserves and ensuring resource succession. In addition, new fields such as gravity flow deposits in slope facies and marlstones in evaporative lagoon facies are worthy of exploration. The establishment of the new models of carbonate sedimentation strongly supports the deployment of oil and gas exploration, and also provides a new direction and ideas for future exploration.

Carbonate oil and gas fields represent a significant component of global hydrocarbon resources, accounting for over 60% of the total conventional reserves. This paper systematically reviews the distribution characteristics of giant carbonate oil and gas fields worldwide. Through analysis of typical fields, it summarizes the primary controlling factors for hydrocarbon accumulation and identifies new frontiers for exploration. The results indicate that these giant fields are predominantly located in regions such as the Persian Gulf Basin in the Middle East, the Pre-Caspian Basin in Central Asia, the Permian Basin in North America, and the Santos Basin in Brazil, with reservoir ages ranging primarily from the Mesozoic to Cenozoic. The key factors controlling hydrocarbon accumulation include: (1) sedimentary background, which determines the scale of source-reservoir-cap rock systems; (2) tectonic and diagenetic modifications, which create large-scale reservoirs; (3) tectonic stability and seal integrity, which are crucial for reservoir preservation. Future exploration should focus on new frontiers such as ultra-deep formations, deep-water environments, complex tectonic zones, and unconventional carbonate reservoirs, which are expected to become vital successors for future resource supply.

Three marine shale formations of the Middle-Upper Permian—the Gufeng Formation (P₂g), the 3^rd member of the Wujiaping Formation (P₃w₃) and the 1^st member of the Dalong Formation (P₃d₁), are well developed in the northeastern Sichuan Basin, representing promising new targets for enhancing shale gas reserves and production. Based on extensive core testing data, this study analyzes their geochemical characteristics, reservoir features and proposes corresponding development strategies to provide theoretical support for shale gas exploration in China. The key findings are as follows: (1) All three shale formations exhibit high organic matter abundance, with average total organic carbon (TOC) contents of 9.82% (P₂g), 6.60% (P₃w₃) and 6.01%(P₃d₁), respectively. The organic matter is classified as type II₁, and the maturity(R_o) exceeds 2.0%, indicating significant hydrocarbon generation potential. The Gufeng Formation is dominated by siliceous shale and calcareous shale facies, whereas P₃w₃ and P₃d₁ primarily consist of siliceous shale and mixed shale facies. The brittleness index of all three formations exceeds 70%. Organic pores are the dominant pore type, with mesopores serving as the primary pore category. (2) The P₃w₃ exhibits well-developed laminated fractures, highest pore connectivity index (average value of 5.17), high porosity and high gas content; the P₂g has moderate pore connectivity index (average value of 2.57), high porosity and gas content; the P₃d₁ shows poor laminated fracture development, the lowest pore connectivity index(average value of 1.69), the lowest porosity value and relatively high gas content.(3) Compared to the Longmaxi Formation in southern Sichuan Basin, these three shale formations are characterized by high TOC content, high brittleness index, high gas content, thin thickness and deep burial depth. Targeted development technologies are thus required. Favorable areas for shale gas enrichment of these three formations are primarily distributed in the southeastern segment of the Kaijiang-Liangping Trough and the Chengkou-Fengjie-Lichuan-Shizhu area of the Chengkou- E'xi Trough.

Taking the Cambrian Xiaoerblak section in the Keping outcrop area as an example, this study aim to clarify the differences in the characteristics and distribution patterns of dolomite reservoirs of the Upper Cambrian Xiaqiulitage Formation in the western Tarim Basin. Based on a systematic analysis of rock thin section, carbon and oxygen isotope compositions, and U-Pb dating, the conclusions are drawn as follows:(1) The Xiaqiulitage Formation, with a total thickness of 350 m, is divided into six members, and is composed of grain dolomite, thrombolite dolomite, stromatolite dolomite, and laminated microbialite dolomite. Seven lithofacies association and two third-order sequences are identified in the Xiaqiulitage Formation, reflecting the overall transition of tidal flat subfacies to inner platform shoal subfacies from bottom to top. (2) The reservoir spaces are dominated by matrix dissolution pores, vugs (dissolution cavities), and intergranular fractures within breccias. The columnar stromatolitic dolomite and thrombolitic dolomite exhibit the best physical properties, followed by grain dolomite, with the overall characteristics of moderate-to-high porosity and moderate-to-low permeability. A comprehensive evaluation indicates that the reservoir properties are optimal in Member 1, Member 2, and Member 6, while Member 5 ranks slightly lower. (3) The dolomite was formed during the early diagenetic stage, and reservoir development is primarily controlled by the combined effects of sedimentary microfacies, unconformity surfaces, and high-frequency sequences. The reservoirs can be classified into two types: unconformity-karst dolomite reservoirs and inner mound-shoal dolomite reservoirs. This research provides critical support for evaluating favorable exploration zones in the Cambrian dolomite plays of the western Tabei area, and offers reliable evidence for hydrocarbon reservoir assessment, particularly in the Xiongying region.

Fault interpretation is one of the core tasks in oil and gas exploration and development. However, with the increase of exploration scale, traditional artificial fault interpretation and conventional fault detection methods are unable to meet practical needs. Deep learning methods provide an important approach for intelligent seismic fault recognition, among which deep network models represented by Unet have achieved many successful cases in this type of task. However, due to the particularity of convolution operations, this method loses some information in the feature extraction process, resulting in the need for further improvement in the accuracy and robustness of fault recognition. In this paper, we design a CNN-Transformer hybrid module and embed it into the Unet network framework, proposing a hybrid network model based on U-CNNformer. The hybrid network model improves the mining ability of both global features and local details in the sample set, overcomes the limitations of the conventional Unet network in weak information correlation in fault recognition, and improves the robustness of the model while ensuring the accuracy of fault recognition. Testing on the publicly available North Sea F3 data and applying with actual data in a certain area of Sichuan Basin in China demonstrate that the proposed hybrid network model not only accurately detects fault features but also provides a more detailed characterization of fault distribution, achieving high-precision intelligent fault recognition with excellent application effectiveness.

The cratonic strike-slip fault zone is an important hydrocarbon accumulation zone in the ultra-deep carbonate rock field of Tarim Basin. At present, the natural energy of the oil reservoirs in the strike-slip fault zone is insufficient, and the decline rate of the oil reserves is fast. It is urgent to deepen the understanding of the geological characteristics of such oil reservoirs, explore new development methods, and investigate countermeasures for enhancing recovery rate. Based on the detailed study of the 12th and 17th fault zones in Fuman Oilfield through comprehensive analysis of outcrops, drilling, seismic surveys, core thin sections, production dynamics, well tests and other data, the types of reservoir space, internal structural characteristics and hydrocarbon accumulation features of the fractured breccia reservoirs are precisely characterized. Appropriate countermeasures for enhancing recovery rate are proposed. The research results indicate: (1) The fractured breccia reservoirs belong to vertical plate-shaped oil reservoirs. The reservoirs develop in the fault core and fracture zone, their reservoir space types are breccia interstitial pores, cavities and structural fractures formed by cataclasis. (2) The ultra-deep fractured breccia reservoirs are initially deposited as tight lithofacies, with very low pre-existing formation porosity and permeability, preserving a low amount of original formation water. There was no significant dissolution of atmospheric water in the later stage, which led to the fractured reservoir bodies having the characteristics of high oil column (up to one thousand meters) and being water-free or having little water content. (3) In terms of geological understanding, detailed description of reservoirs and development methods, three aspects of understanding transformation have been formed: from fault-controlled karst reservoir to fractured breccia reservoir, from description of fault-karst oil reservoir to the internal structure description of fractured breccia oil reservoir, from water injection development to gas injection development.

The Maokou Formation of Middle Permian has huge resource potential and is an important target for natural gas exploration in Sichuan Basin. In recent years, significant exploration breakthroughs have been made in the dolomite of the 2^nd member of Maokou Formation in central Sichuan Basin, and the gas production of several wells has exceeded one million cubic meters, which reveals the huge exploration prospect in this field. However, the genesis of dolomite is still unclear, which restricts the prediction of dolomite distribution. Focusing on the core exploration wells in Hechuan area, a detailed description of the petrological characteristics based on core and thin sections is carried out, and representative samples of dolomite and limestone are selected for carbon oxygen isotope, strontium isotope, rare earth element, and U-Pb dating analysis. Taking into account the geological background, it was clarified that: (1) Dolomite is mainly developed in the middle-upper part of the 2^nd member of Maokou Formation, with a thickness of 1-25 m, and its original rock is grainy limestone. (2) The dolomitization fluid is mainly seawater, and dolomitization occurred in the quasi-contemporaneous period-early burial period. (3) The shoal developed in a relatively paleogeomorphologic high part of the 2^nd member of Maokou Formation was susceptible to syngenetic karstification, and a large fracture-cavern system developed in the phreatic zone. Fracture-cavern system were filled with bioclastic particles, marl and Mg²⁺ rich seawater, and dolomitization occurred during the shallow burial process. Based on the new research results of dolomite genesis, it is clear that the paleogeomorphologic high part is the favorable area of dolomite of the 2^nd member of Maokou Formation, which provides a basis for the prediction of dolomite reservoir distribution in the study area and effectively guides the exploration deployment.

The Ledong gas field group is located near the slope break zone of the Yinggehai Basin, and the gas field has entered the middle and late stages of development, and it is of great significance to clarify the distribution of residual gas for tapping the remaining potential of the gas field. It is important to conduct research on sedimentary facies types, sedimentary models, sand body stacking relationships, and configurations based on rock facies characterization, grain size analysis, logging facies identification, and seismic facies characterization of the 1st member of Yinggehai Formation.Two types of sedimentary facies are identified in the research area, including littoral-shallow marine, and submarine fan. Among them, the littoral-shallow marine subfacies can be further subdivided into three types of sedimentary microfacies: shoreface bar, shoreface beach, and shelf mud.Three types of sedimentary models have been established: progradational shallow marine beach-bar composite model on the gentle shelf slope; slump-reworked bar-filling depositional model at the slope margin; shallow marine gravity-flow slump fan model below the slope break.Three types of sand body stacking relationships have been identified: progradational stacked sand bodies developed above the slope break zone exhibit good connectivity;laterally contacted stacked sand bodies (formed by slump-reworked bar sands) near the slope break show moderate connectivity;vertically isolated submarine fan sands deposited below the slope break display poor connectivity. The slump-reworked bar sand bodies near the slope break zone and the submarine fan-derived sand bodies below the slope break are identified as the most promising potential targets for future gas field development.

Taking the middle and upper sections of the Pinghu Formation on the Pinghu slope in Xihu Sag as an example, by synthesizing the research achievements of coastal sedimentary systems at home and abroad, this study innovatively integrates paleogeomorphology, sedimentary characteristics of tidal flat areas, and coastal sedimentary models to explore their impacts on tidal dynamics and sedimentary system distribution, providing key basis for subsequent large-scale lithologic trap oil and gas exploration and development. Comprehensive application of drilling and logging data, seismic data, and sedimentary process numerical simulation techniques is conducted to simulate the spatio-temporal evolution of the sedimentary system. Through qualitative description and quantitative measurement, the distributions of unique sedimentary units such as tidal channels, tidal gullies, tidal sand ridges, and tidal sand sheets are clarified, the controlling effects of coastal topography and sea-level changes on tidal sedimentary sand bodies are revealed, and three sedimentary models, namely barrier coast, barrier-free underwater low-relief coast, and barrier-free gentle slope coast, are constructed to improve the theoretical framework of coastal sedimentary systems. Further comparative analysis between numerical simulation and actual data shows that barrier coast sand bodies are sheet-like distributed during low sea-level periods, while underwater low-relief coast sand bodies are ribbon-like distributed during high sea-level periods. For the first time, large-scale tidal sand ridges in barrier and underwater low-relief sedimentary environments and restricted tidal channel sand bodies are identified as key targets for oil and gas exploration.

After more than 50 years of exploration, the Santos Basin in Brazil has become the continental margin basin with the most deep-water oil and gas discoveries in the world to date. Based on the primary exploration objectives and the process of oil and gas discoveries, the exploration history of the Santos Basin can be divided into three stages: shallow-water clastic reservoir exploration, deep-water gravity flow sandstone exploration, and pre-salt carbonate reservoir exploration. During the deep-water pre-salt carbonate reservoir exploration phase, some large and giant oil and gas discoveries were discovered, establishing the Santos Basin as a global leader in deep-water hydrocarbon exploration. The exploration in the Santos Basin has always been accompanied by innovation in geological understanding and advances in exploration technology. Particularly in the phase of deep-water pre-salt carbonate reservoir exploration, there was a transition from focusing on giant structural traps in the core exploration areas to the peripheral and outer regions. The innovations in oil and gas geological understanding played a key role in determining the direction of exploration into ultra-deepwater frontiers. These innovations primarily include four aspects: the differential distribution of hydrocarbon source kitchens determined by the tectonic framework during the rift phase, the genesis and distribution characteristics of large-scale reservoirs, the distribution patterns of medium and large scale oil and gas fields, and the distribution characteristics of mantle-derived carbon dioxide. During the exploration of the Santos Basin, major international oil companies were actively involved in the oil and gas exploration bidding. However, they exhibited different exploration strategies, and the drilling results were, on the whole, far below expectations. This not only confirmed the basin´s rich oil and gas potential but also revealed the significant variability in hydrocarbon accumulation and reservoir formation within continental margin basins. As a typical passive continental margin basin, understanding the oil and gas accumulation patterns and key factors in the deep-water regions of the Santos Basin has significant reference value for comprehensively understanding and systematically mastering the petroleum geological characteristics of global continental marginal deep-water basins. It also provides guidance for the expansion of new frontiers in deep-water exploration and optimizing exploration planning.

This study addresses the core issues of unclear sequence architecture and sedimentary evolution patterns of the bioclastic limestone member of the Carboniferous Bachu Formation in eastern Tazhong area, Tarim Basin. Based on a wealth of data, including core, thin section, logging, and geochemical data, we conduct an in-depth analysis of the petrological characteristics of the bioclastic limestone member, construct the sequence stratigraphic framework for this member, and explore its control on sedimentation and reservoir formation. The research findings demonstrate that: (1) The bioclastic limestone member in the eastern Tazhong area represents a mixed siliciclastic-carbonate sedimentation within a marine-terrestrial transitional setting, mainly composed of micritic to peloidal limestone/dolomite, calcarenite/doloarenite to calcirudite/doloyunrudite, mixed rocks, and transitional lithologies, with a relatively high content of terrigenous clastics. The distribution of lithologies exhibits distinct vertical segmentation and lateral zonation patterns. (2) Based on variations in lithology and sedimentary facies, the bioclastic limestone member, along with the underlying Donghe sandstone member, the lower mudstone member, and the overlying middle mudstone member, forms a complete three-order sequence. The bioclastic limestone member itself represents a complete transgressive-regressive sequence, with the middle submember recording the relatively deepest marine flooding conditions during deposition. (3) The eustatic cycles exert a decisive influence on the evolution of sedimentary microfacies and diagenetic processes. The lower and upper submembers, deposited in shallow waters, are dominated by supratidal dolomicrite (dolomudstone) facies within evaporitic tidal flats. During relative sea-level rise in the middle submember, high-energy grain shoal complexes developed within intertidal settings, where superimposed high-frequency exposure events drove meteoric dissolution and penecontemporaneous dolomitization, thereby generating high-quality reservoirs with superior storage capacity. These dolomitized grain shoal and dolomicrite flats with pinprick vugs together constitute the most favorable reservoir facies of the bioclastic limestone member in the eastern Tazhong area, Tarim Basin, and represent the primary targets for future exploration and development.

The interaction between deep-water gravity flow and bottom flow is a currently hot topic in deep-water sedimentary research in the world. This study focuses on the Upper Eocene of the Rovuma Basin in East Africa, utilizing a comprehensive approach integrating drilling and 3D seismic data to investigate this geological topic. The sedimentary architectural elements and evolution characteristics under a high-frequency sequence stratigraphic framework is studied to reconstruct the depositional and evolutionary patterns of the submarine fan under the interaction of gravity and bottom currents in the Upper Eocene. The results show that: (1) The Upper Eocene submarine fan in the study area develops three types of sedimentary architectural elements: deep-water channels, overbanks and lobes. The channels can be further divided into two types: confined deep-water channels and semi-confined unidirectionally migrating channels. (2) The Upper Eocene third-order sequence can be divided into three fourth-order sequences: Ps1, Ps2 and Ps3. Among them, the Ps1 sequence develops a confined deep-water channel-lobe complex, the Ps2 sequence develops a semi-confined unidirectionally migrating channel-lobe complex, and the Ps3 sequence develops a lobe complex. The evolution of these sequences represents a cyclic evolution process within the third-order sequence under the background of continuous rise in sea level, changes in seafloor landform filling, attenuation of gravity flow energy, and relative enhancement of bottom currents.(3) Bottom currents could strip fine-grained materials in gravity flows accumulate on the northern side (downstream side of the bottom current) of the deepwater depositional system, forming asymmetric overbank/drift deposits with positive topography. This, thereby, restricts channels and lobes to southward erosion and deposition, resulting in the Eocene deepwater depositional system and depositional architectural elements that exhibit a unidirectional migration and stacking pattern on the upcurrent side. It is inferred that bottom currents may enhance the reservoir quality of gravity flow deposits.

In recent years, many large-scale biogenic gas reservoirs have been discovered in the world, which has become one of the hotspots of natural gas exploration. Biogenic gas reservoirs are mainly distributed in passive continental margin basin, foreland basin, craton basin, fore-arc basin, and accretionary wedge, etc. The conditions of biogenic gas accumulation in accretionary wedge are complicated due to the intense tectonic activity, and there is a lack of systematic understanding of biogenic gas enrichment rules and main controlling factors in accretionary wedge. Based on 2D seismic, well data, we discuss the biogenic gas accumulation conditions in Barbados accretionary wedge, north of South America and define the hydrocarbon migration and accumulation model, and furtherly reveal the law of oil and gas enrichment and point out the favorable exploration direction. The results show that: (1) From west to east, the inner (western) depression, the central uplift, and the outer (eastern) thrust zone develop successively, and the inner zone develops the large sag. (2) The thick mudstone in the large sag provides sufficient biogenic gas source. Large channel complexes, channel-levee complexes, channel-lobe complexes, and lobes are mainly developed in western depression, which has a good relationship with traps. Early high relief thrust-faulted anticline is located in the convergence area of oil and gas, which is conducive to efficient biogenic gas accumulation. (3) Since the Pliocene, under the compression of the Caribbean Plate, the central uplift belt has widely developed mud diapirs, forming numerous mud diapir-related structural traps. The continuous activity of these mud diapirs persists to the present day. The activity of late-stage mud diapirs has led to the destruction of biogenic gas reservoirs, resulting in the failure of all drilling attempts on the flanks of the mud diapirs. So late preservation conditions are the key factors for biogenic gas accumulation. (4) The model of Biogenic gas self-generation and self-storage or lower-generation and upper-storage is established. The western depression has favorable conditions for the formation of biogenic gas reservoirs and is a favorable exploration direction.

The tight gas resource potential of the Lower Jurassic Ahe Formation in Dibei area of the eastern Kuqa Depression is enormous, making it a promising region for increasing oil and gas reserves and production. For a long time, the coupling relationship between sweet spot model and oil and gas enrichment of tight sandstone reservoir in Ahe Formation is unclear, which restricts the efficient exploration and development of tight oil and gas reservoirs.Based on microscopic reservoir characterization, geological modeling, fault-fracture characterization and reservoir analysis, this paper investigates the sweet spot characteristics and hydrocarbon enrichment patterns of tight sandstone reservoirs in the Ahe Formation, and evaluates their resource potential. The study reveals that the Ahe Formation reservoirs exhibit an alternating distribution of tight layers and low-porosity/high-permeability zones laterally. Reservoir properties are significantly enhanced by fault-fracture modification, developing sweet spot areas at four hierarchical scales. The fracture-pore systems controlled by class I-II faults extend east-west direction, characterized by large scale and favorable porosity-permeability properties. The fracture-pore systems controlled by class Ⅲ-Ⅳ faults/fractures are small in scale and pinch out within tight sandstones. The first hydrocarbon charging event in the Ahe Formation reservoirs occurred between 18 and 12 Ma, with porosity ranging from 15% to 18% during this phase. The primary charging fluid was crude oil, which accumulated in structural highs to form conventional oil reservoirs. However, these reservoirs were subsequently severely disrupted, leading to complete dissipation of the accumulated hydrocarbons. The second hydrocarbon charging phase commenced since 5 Ma, during which the reservoir underwent rapid densification, with porosity reduced to 6%-8%. Natural gas efficiently migrated along faults and fractures, accumulating preferentially within sweet spot zones of the reservoir. Class Ⅲ and Ⅳ faults/fractures zones establish effective connectivity between sandstone units within the Ahe Formation, forming optimal configurations with adjacent tight reservoirs and overlying mudstones. These structural features constitute critical controls on both trap effectiveness and hydrocarbon accumulation. The favorable area for oil and gas enrichment in tight sandstone of the Ahe Formation can reach 106 km², mainly concentrated in the central and southern platform areas of the Dibei Slope. The lithological trap resources of natural gas are 1 699 × 10⁸ m³ and petroleum are 778 × 10⁴ t.

In recent years, natural gas exploration breakthrough has been made in the Ordovician Majiagou Formation of Ordos Basin, but the formation and evolution of natural gas have not been thoroughly studied. Taking Daniudi gas field as an example, the typical characteristics of oil-cracked gas in Majiagou Formation are determined through the identification of bitumen in the core and thin section, the occurrence of hydrocarbon inclusions and Raman spectroscopy testing, and the analysis of geochemical data of natural gas. The formation conditions of oil-cracked gas are comprehensively analyzed, and the formation and evolution process of oil-cracked gas in Majiagou Formation are analyzed through the simulation of burial history and thermal history. The results show that: (1) Bitumen filling with diverse occurrences is found in the fractured porous reservoir of Majiagou Formation, and it is a dry bitumen with high degree of thermal evolution. Three phase hydrocarbon inclusions of oil, gas and bitumen are captured in calcite veins of Majiagou Formation, which confirms the existence of oil cracking gas process. (2) Based on the crossplot of geochemical index such as ln(C₁/C₂) and ln(C₂/C₃) of natural gas, it shows that the internal natural gas of Majiagou Formation is mainly oil-cracked gas. (3) During the deposition period of 3^rd member of Majiagou Formation, Daniudi and its surrounding areas were situated at the margin of a saline depression, where thick source rocks of argillaceous dolomite and dolomitic mudstone developed with interbedded evaporates, creating favorable conditions for thermochemical sulfate reduction (TSR). (4) In the Early Jurassic, source rocks produced a large amount of oil. Under the effect of the relatively high paleotemperature in the Early Cretaceous, high-temperature oil cracking occurred, and TSR reaction occurred with significantly increased H₂S content in the natural gas of O₁m₅⁵-O₁m₅⁶ of Majiagou Formation in Daniudi gas field. (5) In Daniudi and surrounding areas, the source rocks of Majiagou Formation became mature earlier in the south and later in the north, and natural gas mainly migrated and accumulated from south to north along the strike-slip faults. This study has certain significance for the internal gas exploration of Majiagou Formation in Ordos Basin.

The fault-controlled carbonate rocks of the Fuman Oilfield in the Tarim Basin have attracted much attention due to the continuous discovery of ultra-deep oil and gas, and there is an urgent need to further clarify the role of hydrothermal fluids in modifying such reservoirs. Based on seismic data interpretation, combined with field outcrop observation, core and thin section analysis, geochemical analysis, and production characteristic analysis, an in-depth study is conducted on the hydrothermal alteration effects on the Ordovician ultra-deep fault-controlled reservoirs in the Fuman Oilfield of the Tarim Basin.The study find that there are three types of hydrothermal alteration effects on the ultra-deep Ordovician reservoirs in the Fuman Oilfield: ⑴The dissolution-storage enhancement effect, which develops in an open-semi-open environment. On the one hand, the high temperature of hydrothermal fluids accelerates the chemical reaction rate and promotes mineral dissolution; on the other hand, in the open-semi-open environment, hydrothermal fluids carry the dissolved substances out of the reservoir system, forming good reservoir spaces. (2) The cementation-dissolution synergistic reservoir-controlling effect, which occurs in a closed system with weak late tectonic stress. The coupling of fault activity stages and fluid evolution leads to the upper part being dominated by cementation and filling (enhanced sealing) and the lower part being dominated by dissolution and expansion (improved reservoir performance), forming a dynamic equilibrium structure of "upper blocking and lower storing". (3) The cementation-brittle transformation and fracturing effect, that is, during diagenesis, the cementation caused by hydrothermal fluids enhances the brittleness of the rocks, and subsequent fracturing occurs in the dendritic internal structure of strike-slip faults under the action of tectonic stress or fluid pressure imbalance, forming new reservoirs and enhancing the seepage capacity of the oil reservoir.This study on the alteration effects of ultra-deep hydrothermal fluids on reservoirs in the Fuman Oilfield of the Tarim Basin has deepened the understanding on the mechanism of synergistic reservoir control by hydrothermal fluids and faults, revealed the development law of strong heterogeneity in ultra-deep fault-controlled reservoirs, and further clarified the exploration direction of such reservoirs.

The microbial carbonates of the Lower Cretaceous Barra Velha Formation in the Santos Basin, Brazil, primarily formed in a high-salinity alkaline depositional environment, and have recently become a hotspot for hydrocarbon exploration and development in deep-water areas. However, research on the characteristics of microbial carbonate reservoirs formed in such unique environment is relatively limited and controlling factors of reservoir formation remains poorly understood. Based on integrated core samples, thin sections, well logs, and petrophysical test data, this study systematically investigates the lithofacies, reservoir space types, and physical properties of microbial carbonates in the basin. It clarifies the diagenetic sequence and pore evolution of the reservoirs and explores the main controlling factors and models for the development of high-quality reservoirs. The research results show that: (1) The main rock types of microbial carbonate reservoirs of the Lower Cretaceous Barra Velha Formation in the Santos Basin include stromatolite, spherulitite, laminite, rudstone, grainstone and breccia. The formation can be divided into two third-order sequences, primarily consisting of four microfacies types: microbial reef, grain shoal, microbial spherulitic shoal, and inter-shoal deposits. (2) The reservoir space is mainly composed of biological framework pore, framework dissolution pore, intergranular pore, intergranular dissolution pore, intragranular dissolution pore, intercrystalline pore, and dissolution fracture. Porosity and permeability generally exhibit a positive correlation, indicating the dominance of pore-type reservoirs. Statistics show that the microbial reef and grain shoal microfacies have better reservoir properties, while the microbial spherulitic shoal and inter-shoal microfacies show relatively poorer reservoir quality. (3) The diagenetic sequence and pore evolution of microbial carbonate reservoirs have been clarified. In the early diagenetic stage, meteoric water dissolution and dolomitization played constructive roles in reservoir evolution. In contrast, mid-to-late hydrothermal activity led to silica filling of reservoir pores particularly in areas adjacent to faults, which not only damaged the reservoir but also increased reservoir heterogeneity. (4) Paleoclimate, paleo-water condition, sequence stratigraphy, and sedimentary microfacies types are the main factors controlling the development and distribution of high-quality microbial carbonate reservoirs. Combined with diagenetic evolution, an evolution model of microbial carbonate reservoirs has been established in this study.

For the Carboniferous Huanglong Formation, an important natural gas production layer in Sichuan Basin, in low-relief structural zone on the west side of Huayingshan Fault, there are still problems of unclear accumulation conditions and undetermined favorable exploration zones due to low exploration degree. Based on exploration wells, 2D and 3D seismic data, a new round of evaluation is conducted on the distribution of strata, lithofacies paleogeography, and natural gas accumulation conditions of Huanglong Formation on the west side of Huayingshan Fault. The results show that: (1) The residual strata of Huanglong Formation with thickness mainly between 10-40 m are widely distributed (about 13 100 km²), and about 4 000 km² according to the new seismic interpretation is added in the northern Sichuan Basin. (2) The intertidal shoal dolomites are widely developed (about 8 200 km²), mainly in the Huanglong Member 2, followed by the Huanglong Member 3. The newly discovered Pingchang-Bazhong shoal belt covers an area of about 2 000 km². The thickness of dolomite reservoir of the shoal facies in HuangLong Member 2 is mainly 2-20 m. The reservoir has good physical properties, with an average porosity of 3.90%. (3) The source rocks of Wufeng Formation-Longmaxi Formation in the northern Sichuan Basin are widely developed covering an area of about 25 000 km², and the total thickness is 50-150 m in which the high-quality is 10-60 m. The source rocks of Wufeng Formation-Longmaxi Formation and the reservoirs of Huanglong Formation form favorable reservoir combination of lower generation and upper storage. (4) Controlled by the paleo-uplift slope zone, strata denudation zone, and large fault zone, the Huanglong Formation has developed two large trap groups, i.e., Pingchang-Bazhong, and Guang'an-Quxian, with diverse trap types dominated by lithological-stratigraphic traps and good preservation conditions. Four favorable exploration areas are predicted, indicating a promising prospect for natural gas exploration.

The recent exploration discoveries in Luzhou area indicate that the reef-shoal body of the Silurian Shiniulan Formation has certain potential for reservoir formation. A systematic study based on drilling, outcrop, and 3D seismic data is conducted to explore the development characteristics and exploration significance of the reef-shoal body of Shiniulan Formation. The results indicate that: (1) Reef/bioclastic limestone mainly develops at the top of the first member of Shiniulan Formation, with a thickness ranging from 6 to 40 meters, characterized by moderate-strong amplitude and medium-high frequency seismic reflection character. (2) Affected by the ancient uplift in central Sichuan, the first member of the Shiniulan Formation is developed at mixed tidal flats and intra-platform depressions, forming contiguous tidal edge reefs and shoals on the high terrain of the mixed tidal flats. At some high belts of the intra-platform depressions, intra-platform reefs/bioclastic shoals are developed. (3) The reservoir formation model of Shiniulan Formation is characterized by "near-source hydrocarbon generation, fault-mediated migration, lower-generation and upper-reservoir storage, and composite accumulation". The high-quality hydrocarbon source rocks of the Longmaxi Formation, the reef-shoal reservoir of the first member of Shiniulan Formation, the mudstone of the second member of Shiniulan Formation and the overlying strata form a good source rock-reservoir-caprock combination. The complex network fault system provides conditions for oil and gas migration, and the oil and gas filling period matches the trap formation period (P-K), laying the foundation for large-scale oil and gas accumulation. The Shiniulan Formation reef-shoal body is an important oil and gas exploration field worthy of attention.

Diagenesis of reservoirs affects pore development, distribution and reservoir quality. Relevant studies on the Middle Triassic Leikoupo Formation in central Western Sichuan Basin are still blank. In order to reveal the diagenetic evolution characteristics of dolomite reservoirs in the study area and their influence on reservoir quality, and to provide a theoretical basis for the exploration of carbonate oil and gas, the study on the dolomite diagenesis of Leikou Formation in western Sichuan Basin is systematically analyzed on the basis of data analysis such as core and thin section observations, dolomite order degree analysis, fluid inclusions and carbon-oxygen stable isotope tests. The results show that: (1) The Leikoupo Formation in central Western Sichuan mainly develops two different types of dolomite: micritic dolomite and micritic algal clast dolomite. The low degree of ordering and low formation temperature of the dolomite crystals indicate that they were formed by penecontemporaneous dolomitization. The reservoir spaces mainly consist of dissolved pores developed along algal frameworks, intergranular pores, and tectonic breccia interstices. (2) The dolomite in the study area has mainly undergone diagenetic processes such as fracturing, dolomitization, dedolomitization, dissolution, micritization, cementation, and surface-induced demineralization. Among them, structural fracture and dissolution play an improving role in the physical properties of the reservoir. Deep dissolution is the fundamental factor for the development of deep secondary pores. (3) The correlation between the development characteristics of dissolution pores and structural breccia and structural fractures is confirmed: acidic fluids were injected along the fracture space into the remaining pore development areas such as sandy shoal and the framework of the algal layer to form secondary dissolution pores in the late Indosinian stage. Vertical fissures and late structural breccia were formed in the early stage of the Himalayan Movement, and late dissolution and calcite vein filling occurred. Horizontal fractures formed in the late Himalayan period, further improving the physical properties of the reservoir. The research has for the first time clarified the diagenetic sequence and pore evolution model of the dolomite reservoir of the Leikoupo Formation in central Western Sichuan Basin, and proposes a three-stage reservoir control mechanism of "structural fracture-fluid dissolution-fracture modification", providing new geological basis for the exploration of the Leikoupo Formation.

The extensional-convergent tectonic cycle is commonly developed in the carbonate strata of the middle-lower assemblages within small cratons in central and western China. It not only governs the sedimentary differentiation and filling processes but also provides the core driving mechanism for the development and spatio-temporal arrangement of fundamental petroleum geological elements in deep-ultra-deep domains.Taking the Neoproterozoic-Ordovician in the Tarim Basin as an example,by leveraging 42 newly acquired and spliced seismic lines, a 3D data volume spanning 56 000 km² in the Tazhong-Tabei area, more than 70 wells, C-O isotope data (sampled at 5-10 m intervals), and over ten thousand cuttings (core) thin sections, we reconstruct the tectonic-paleogeographic background during key tectonic transformation (sub) stages. Subsequently, lithofacies paleogeographic maps are meticulously compiled in sequence units to clarify the platform type conversions and sedimentary differentiation characteristics within the extensional-convergent cycle and to determine the reservoir-forming assemblages.The results indicate that: (1) The differential sedimentary filling of two types of Nanhua Period paleo-rifts, combined with the inherited paleo-uplifts and the (syndepositional) paleo-uplifts formed by convergent compression in the Middle-Late Ordovician, jointly constitute the foundation for tectonic-paleogeogeographic differentiation. (2) The Sinian-Ordovician can be divided into one first-order sequence and four second-order tectonic sequences, corresponding respectively to four evolutionary stages: the rift-depression transition stage, the cratonic extensional construction stage, the extensional-convergent transition stage, and the convergent strong differentiation-drowned platform stage. During this period, the tectonic-paleogeographic background and paleo-sea level fluctuations controlled the orderly succession and development of muddy slopes, carbonate slopes, rimmed platforms, and drowned platforms. (3) Six sets of large-scale source rocks were developed within the extension-convergence cycle. These source rocks, together with the following five assemblages, constitute five types of source-reservoir-cap assemblages: mudstone of the Cambrian Yuertusi Formation-dolomite of the Upper Sinian, gypsum-salt rock of the Cambrian Miaolingian Series-dolomite of the Cambrian Series 2, tight carbonate rocks and mudstone of the Lower Ordovician-weathered crust of dolomite of the Cambrian Furongian Series, Sangtamu mudstone of the Upper Ordovician-fault-controlled karst weathered crust of the Middle-Upper Ordovician and slope-facies mudstone-collapse body of the Cambrian Furongian Series.

The Volga-Urals Basin is a typical foreland basin on the Eastern European Platform, accounting for a significant proportion of global conventional and unconventional oil and gas reserves. However, the understanding of its basin formation and reservoir accumulation remains limited. Through systematic investigation of geological data, the evolution of the basin and its lithofacies paleogeographic characteristics are comprehensively analyzed based on the sedimentary filling features during different Pre-Mesozoic geological periods. The results show that: (1) Under the influence of different tectonic stresses such as tensional stress and compressional stress, the Volga Ural Basin underwent tectonic evolutionary stages of extensional and compressional regimes, developing four prototype basin types/stages: intracontinental rift, passive continental margin, back-arc depression, and back-arc foreland basin. (2) During different tectonic evolution processes, the basin has undergone multiple-cycle changes from terrestrial to marine and back to terrestrial. During the Meso-Neoproterozoic, the basin remained generally stable with sedimentation confined to its eastern region, dominated by terrestrial clastic deposits; in the Early Ordovician, the opening of the Ural Ocean led to a marine transgression across the East European Platform, characterized primarily by shallow marine carbonates; beginning in the Devonian, the basin underwent multiple regressive-transgressive cycles; by the end of the Permian, the entire basin was fully uplifted and subjected to erosion. (3) The basin developed four petroleum systems, with the Domanik Formation serving as the primary source rock. The transitional facies and shallow marine facies developed during the transgressive phase constitute two critical hydrocarbon reservoir units in the basin. Muhanovo-Erohovsk Sag and Kashan-Kama Depression are respectively the key area for unconventional and conventional oil and gas exploration in the future. The research findings provide a critical foundation for the evaluation of overseas oil and gas projects and the implementation of exploration and development practices.

Marine carbonates have played a crucial role in the over 70-year natural gas exploration history of the Sichuan Basin, and will remain a primary target field for natural gas exploration and development for a long time to come. Based on the study of tectonic and lithofaies paleogeographic evolution of the entire marine strata, a systematic analysis of the macro-control factors and the influencing factors of the reservoirs of different formations has been conducted in order to explicitly define the distribution and exploration directions of large scale high-quality marine carbonate reservoirs in the Sichuan Basin. The study concludes that: (1) The marine strata of Sichuan Basin has undergone four major tectonic cycles, with 13 significant tectonic movements. Of these, two tension-dominated movements created the paleogeographic pattern of the trough-platform alternation, while eleven uplift-dominated movements governed the sedimentary characteristics of the large platform/ramp. (2) The conventional marine carbonate reservoirs in the Sichuan Basin can be simply divided into two main types: sedimentary facies-controlled reservoir and karst reservoir. The development of high-quality reservoirs is macroscopically controlled by tectonic processes, mainly distributed in the inclined areas of ancient uplifts and the geomorphic high zone on both sides of the ancient rifts. (3) Six potential areas for large-scale exploration of carbonate rocks in the future in the Sichuan Basin are proposed: the platform-margin zone of the Dengying Formation on the west side of the Deyang-Anyue rift trough, the dolomitization shoal of the Lower Paleozoic on the east edge of paleo-uplift in the central Sichuan Basin, the multi-layered platform-margin zone of the Upper Paleozoic on the west side of the Sichuan Basin, the dolomitization shoal of the lower part of the lower second member of Maokou Formation in Xuanhan-Wanzhou area of the eastern Sichuan Basin, the dolomitization shoal of the third member of Maokou Formation in Yilong-Quxian area of the eastern Sichuan Basin, and reef-shoal limestones of the Changxing Formation along and within the Pengxi-Wusheng intra-platform sag.

Carbonate rocks in Africa are characterized by extensive distribution along continental margins and scattered occurrences in the continent. Carbonate rocks are primarily distributed in rift basins and continental margin rift basins along the Tethyan margin of North Africa. Due to widespread marine transgressions during the Cretaceous and Cenozoic, North Africa remained in a passive margin or epeiric sea environment, in favor of extensive carbonate deposition. They also occur in passive continental margin basins of West and East Africa, although with limited continuity and thickness due to narrow continental shelves and high fluvial input. Scattered carbonate deposits are found within intraplate rifts and ancient cratonic basins, which are dominated by mixed clastic-carbonate sedimentation. Carbonate rocks are concentrated in the Cretaceous and Cenozoic, with localized occurrences in the Jurassic, and extremely limited prior to the Paleozoic. The accumulation conditions in African carbonate basins can be classified into three types: (1) The Sirte Basin and Pelagian Basin have vertical stacking of mudstones, carbonates, and evaporites due to multiple cycles of rifting, inversion, and sea-level fluctuations, indicating excellent petroleum systems in the Cretaceous and Cenozoic sequences. (2) The Kwanza Basin and Lower Congo Basin of West Africa have petroleum assemblage of lacustrine source rocks, lacustrine carbonates, and overlying evaporite seals, in addition, reservoirs with underlying lacustrine source rocks, overlying marine carbonates and mudstones developed. (3) The Eratosthenes isolated platform generated biogenic reef due to the inherited paleo-uplifts and suitable sea levels. There has an appropriate hydrocarbon system of Upper Cretaceous deep-sea source rocks, reef carbonate reservoirs, and Miocene evaporite seals.

Taking the marine shale of the Permian Wujiaping Formation in the Kaijiang-Liangping Trough, Sichuan Basin as the research object, this study quantitatively characterizes the pore structure characteristics of different shale lithofacies through experimental analyses such as X-ray diffraction (XRD), gas adsorption, and high-pressure mercury intrusion (HPMI). Based on equations like V-S and FHH, the fractal dimensions of shale pores are calculated to reveal the pore heterogeneity characteristics of shale reservoirs. Furthermore, the influencing factors and geological significance of pore development heterogeneity in different lithofacies are clarified. The results show that: (1) The lower part of the Wujiaping Formation consists of argillaceous shale, which transitions upward into mixed shale and eventually evolves into siliceous shale in the upper section. Correspondingly, the dominant pore types shift progressively from clay mineral intercrystalline pores to dissolution pores, brittle mineral intercrystalline pores, and organic matter pores. (2) The pores of siliceous shale are dominated by nanoscale organic pores, and their development characteristics are controlled by the distribution morphology and abundance differences of organic matter, showing significant heterogeneity. This results in the highest fractal dimension of micropores in siliceous shales. The mixed shale primarily contains mesopore-scale intercrystalline and dissolution pores, with pore development strongly influenced by diagenetic processes and exhibiting a discrete distribution, leading to the highest fractal dimension of mesopores in this lithofacies. Clay minerals are prone to deformation due to compaction, which makes argillaceous shale highly heterogeneous at the macropore-scale. (3) The TOC content has the greatest influence on the mesopore fractal dimension of siliceous shale, while the macropore fractal dimension increases with the increase of clay mineral content. Comprehensive analysis suggests that highly to moderately organic-rich siliceous shale has the highest overall fractal dimension and strongest adsorption effect on shale gas, making it the dominant lithofacies of the Wujiaping Formation in the Kaijiang-Liangping Trough.

It has been proved that 100-million-ton class oilfield cluster in southwestern Huizhou Sag has an important relationship with the development of high-quality source rocks in Wenchang Formation. The controlling factors of high-quality source rocks in southwest area of Huizhou Sag are not clear enough, which is not conducive to guide the petroleum exploration of peripheral sags. Based on the difference analysis of organic geochemical characteristics of high-quality source rocks, the controlling factors for the development of high-quality source rocks in southwestern Huizhou Sag are studied from the aspects of structure, sedimentation, organic matter sources and preservation conditions. The results show that: (1) The scale and distribution of high-quality source rocks in southwestern Huizhou Sag are controlled by tectonic activities and source supply, especially, during the depositional period, a relatively large fault throw and a low source-to-sink ratio are conducive to the development of high-quality source rocks. The tectonic activity controlled the migration of the subsidence center and sedimentation center from south to north, with HZ26 sub-sag in the early stage and XJ24 sub-sag in the late stage as the central area respectively. (2) The quality of high-quality source rocks depends on the source of organic matter and preservation conditions. The aquatic algal dominance, brackish water-fresh water and hypoxic reduction preservation conditions during Wenchang Member 4 period are more conducive to the development of high-quality source rocks. (3) Strong fault activity, limited distribution of sedimentary sand bodies, input of oil-prone aquatic-terrestrial organic matter, brackish water and strong anoxic environment are important controlling factors for the development of high-quality source rocks in HZ26 sub-sag. This study helps to further understand the potential of source rocks in peripheral sub-sags, and provide important support for the exploration of potential hydrocarbon-rich sags.

The carbonate platforms that have been widely developed in the South China Sea during the Cenozoic Era not only contain abundant oil and gas resources, but also record important paleo-climate and paleo-environmental information, which are of great scientific significance for understanding the regional tectonic evolution and sedimentary responses of the South China Sea(SCS). Based on the drilling data and high-resolution seismic interpretation, this paper systematically analyzes the spatiotemporal distribution characteristics of the Cenozoic carbonate platforms developed in the South China Sea, and also discusses the synergistic controls of tectonic paleogeography, relative sea-level fluctuations, sediment supply, and paleoclimate on the development and distribution of the carbonate platform under compressional, extensional, and strike-slip tectonic settings, corresponding to the subduction and cessation of the Paleo-South China Sea, the progressive expansion of the Neo-South China Sea, and the strike-slip fault system along the western of the SCS. The research reveals that: (1) Based on the tectonic stress conditions, the Cenozoic carbonate platforms in the SCS can be classified into five major platform groups: the Dongsha platform group in the northern SCS, the Guangle-Xisha platform group along the western margin, the Wan′an-Zengxi slope platform group in the southwestern margin, the Luconia platform in the southern margin, and the Liyue-Palawan platform group in the southeastern margin of the SCS, exhibiting a general pattern of "the southern carbonate platforms developed earlier than the north, the eastern carbonate platforms developed earlier than the west, and most of them mainly developed during the Miocene". (2) Based on regional tectonic settings and ocean-continent position variations, the Cenozoic carbonate platforms in the SCS are classified into three types tectonic settings:compressional, extensional, and strike-slip, under each tectonic setting both shelf-margin platforms and isolated platforms are developed. The distribution of the Cenozoic carbonate platforms in the SCS was primarily controlled by regional tectonic activities and fault systems, terrestrial clastic sediment supply, and relative sea level fluctuations. The tectonic setting and fault systems determine the location and basic types of the platforms, the substantial input of terrigenous clastics from large river-delta systems significantly inhibits the development of shelf-margin carbonate platforms, while exerting limited impact on isolated platforms, and the relative sea-level fluctuations control accommodation space changes, thereby regulating the growth patterns, structural evolution, and spatial distribution of biogenic reefs. This study provides critical theoretical support for deep-water hydrocarbon exploration, global climate change research, and oceanic carbon sequestration.

Kwanza Basin, located in Angola and its adjacent offshore area along the West African coast, is a typical passive continental margin salt-bearing basin. It comprises three major structural layers: pre-salt structural layer, salt structural layer, and suprasalt structural layer. The pre-salt Cretaceous lacustrine carbonate rocks represent the primary target for hydrocarbon exploration in the basin. The pre-salt structural layer exhibits a tectonic pattern of alternating depressions and uplifts, which can be divided into the Inner Rift Zone, Central Uplift Zone, and Outer Rift Zone from east to west. The hydrocarbon accumulation mechanism in pre-salt lacustrine carbonate rocks is characterized by "rift-controlled source rocks, uplift-controlled reservoirs, salt-controlled seals, and high-quality reservoirs controlling accumulation". The Central Uplift Zone, with well-developed basement uplifts, not only facilitates trap formation and carbonate reservoir development but also serves as the migration pathway for hydrocarbons, making it the most favorable area for pre-salt Cretaceous carbonate reservoir accumulation. The presence of high-quality reservoirs is critical for successful exploration. Based on newly acquired seismic and drilling data, this study investigates the factors influencing the differential distribution of pre-salt lacustrine carbonate reservoirs. The analysis further narrows down the prospective exploration areas for subsalt hydrocarbon plays in the Kwanza Basin to the northern part of the Central Uplift Zone, providing guidance for regional evaluation and exploration target selection.

The Asmari Formation in Iraq B Oilfield was deposited in a remnant ocean basin environment formed during the closure process of the Neo-Tethys Ocean. Influenced by the intermittent uplift of the Arabian Shield from the Oligocene to Miocene, the study area developed a multi-stage terrigenous clastic supply system. Under the depositional background of a gentle slope, frequent sea-level fluctuations have led to complex mixed sedimentary characteristics of sandstone, dolomite, limestone, and mixed rocks in vertical and planar distributions, whose lithological distribution laws remain to be further clarified. This study takes Iraq B Oilfield as the research object, and systematically reveals the main controlling factors of complex lithology development under the gentle slope background through detailed core observation, thin-section microscopic analysis, and comprehensive interpretation of drilling and logging data. The research has achieved the following understandings: (1) The lithologies of the Asmari Formation can be scientifically classified into three major categories: carbonate rocks, mixed rocks, and terrigenous clastic rocks. Among them, mixed rocks are further subdivided into 8 types based on the 50% ternary classification nomenclature; seven typical lithofacies combination sequences are identified through the coupling analysis of petrological characteristics and logging responses. (2) The spatial distribution of lithofacies shows significant zonation: the northwestern and southeastern regions of the study area are dominated by carbonate facies, the proportion of clastic facies in the central part increases significantly, and the mixed rock facies account for a large proportion in the remaining transition zones. (3) The paleogeomorphology of the study area presents a gentle slope pattern of "low in the northwest and southeast parts and high in the central part". The comprehensive tectonic-sedimentary analysis shows that terrigenous clastic sediments are mainly developed in the paleo-uplift area, carbonate sediments are developed in the paleo-depression area, and mixed sediments are dominant in the transitional slope zone. Finally, a development model of complex lithology controlled by three factors of "paleogeomorphic form—sea-level fluctuation—material source supply" under the gentle slope background is established.

The Permian System in the southern Sichuan Basin serves as the primary target for major natural gas reserve growth in the region. Recent significant breakthroughs in syncline zone have demonstrated that high-yield gas reservoirs in southern Sichuan Basin are not completely controlled by positive structural belts. Instead, strike-slip faults have some control effects on karst paleogeomorphology, high-quality reservoir development and natural gas enrichment in southern Sichuan Basin. However, because the large fold-thrust zones on the shallow surface result in the low seismic resolution and the weak seismic reflection, the strike-slip fault and the characteristics are difficult to determine, and the controlling effect on natural gas enrichment and high yield is unknown, which seriously restricts the exploration and development of fault-controlled gas reservoirs in this area. Therefore, based on artificial intelligence fault identification technology, this paper carries out the identification of deep strike-slip faults, determines the identification marks of strike-slip faults, implements the distribution and characteristics of strike-slip faults in southern Sichuan Basin. Moreover, the controlling effect of strike-slip faults on high-yield gas reservoirs is analyzed based on actual drilling data. The results show that: (1) The artificial intelligence method based on deep learning can improve the identification accuracy of deep hidden strike-slip faults, and can effectively identify hidden strike-slip faults under thrust structures in southern Sichuan Basin. (2) Four planar identification marks and five sectional markers for strike-slip faults in southern Sichuan Basin are defined, thus verifying the development of a rhombus strike-slip fault system in the pre-Permian strata, with a total length of 940 km. (3) The strike-slip fault in southern Sichuan Basin has obvious classification, stratification and staging characteristics. There develop various types of structure such as linear structure, en echelon structure, flower structure and fault horst. Under the geological background of multi-stage extension-convergence, the strike-slip faults develop inheritively from the tension-torsion of the Sinian-Cambrian to the compression-torsional of the Upper Cambrian-Upper Ordovician on the basis of the weak zone of the early basement. (4) The strike-slip fault can connect multiple sets of source rocks in the Cambrian and Silurian, which plays an important role in controlling oil and gas migration and accumulation, and controls the distribution of high-yielding gas reservoirs of the Permian Maokou Formation together with the Permian reverse fault. Deep Cambrian-Ordovician strike-slip faults are a key factor for the high enrichment and productivity of fracture-cave type gas reservoirs controlled by faults in southern Sichuan Basin.

The Lower Paleozoic marine carbonate rocks in the Ordos Basin represent a critical natural gas exploration target in China. However, problems such as strong reservoir heterogeneity and complex hydrocarbon accumulation controlling factors have severely restricted large-scale and efficient exploration and development. This study integrates the latest exploration results with regional seismic profiles, focusing on key scientific issues such as lithofacies paleogeographic evolution, genetic types and controlling factors of reservoirs, and source-reservoir configurations, to systematically investigate the distribution patterns of high-quality carbonate reservoirs and evaluate their exploration potential. The main findings are as follows: (1) The Early Paleozoic sedimentary environment underwent a complete evolutionary sequence from mixed sedimentary shelf (Mantou to Xuzhuang Formation) to carbonate ramps (Zhangxia to Majiagou Formation) and finally to rimmed platforms (Upper Majiagou Formation). Among these, the inner ramp grain shoal facies belts around paleo-uplifts and marine basins exhibit the most favorable reservoir properties. (2) Reservoir development is jointly controlled by depositional microfacies, penecontemporaneous dissolution, supergene karstification, and dolomitization. Five types of reservoirs are identified in the Cambrian-Ordovician succession: grain shoal, algal mound, bioturbated, moldic pore, and dissolution vug types. These reservoirs are predominantly distributed along paleo-uplifts, basin margins and slope breaks. (3) Based on comprehensive analysis of tectonic-sedimentary framework, source-reservoir relationships, and sealing conditions, three highly prospective exploration zones are delineated: the eastern Wuyin marine basin, both flanks of the Yitong marine basin, and the western Shenmu-Mizhi platform depression, with a total area of 10.5×10⁴ km². This study provides critical theoretical support and practical guidance for gas exploration in marine carbonate rocks of the Ordos Basin.

Large carbonate hydrocarbon fields have long been a global research focus. Statistical analysis of IHS data reveals that Africa's giant carbonate oil and gas fields are mainly distributed in five basins: the Sirte, Pelagian, and Eratosthenes basins in North Africa, and the Lower Congo and Kwanza basins in West Africa. Among them, Sirte Basin accounts for 48.2% of Africa's total carbonate oil and gas reserves, making it the most prolific. Through detailed analysis of 19 large carbonate oil and gas fields, the conclusions are drawn as following: (1) The passive-margin marine transgressions associated with the Late Cretaceous-Eocene opening of the Neo-Tethys Ocean and South Atlantic are prerequisites for large-scale hydrocarbon accumulation in carbonate rocks, with the main reservoirs developed in the Cretaceous, Paleocene, and Eocene strata. (2) Unlike deep-water carbonate rocks, the shallow marine sedimentary environment and low latitude warm and humid climate after the breakup of Gondwana continent control the scale distribution of reservoirs and source rocks, forming various types of reservoirs mainly composed of bioclastic limestone, with dolomite, foraminifera limestone, oolitic limestone, and reef limestone as secondary reservoirs, and high-quality source rocks mainly composed of shallow marine shale. (3) During the base-level rise period (lowstand to transgressive system tracts), multiple sets of marine shale (source)-carbonate rock (reservoir)-shale (cap) combinations tend to develop. Subsequently, through sedimentary burial and tectonic processes, structural traps and stratigraphic-lithologic traps are primarily formed, leading to hydrocarbon accumulation. (4) The widely developed limestones, grainstones, and dolomites, along with diagenetic processes, governs the effective reservoirs and physical properties of large carbonate oil and gas fields. Large oil reservoirs are characterized by moderate to high porosity and moderate to low permeability, whereas large gas reservoirs typically exhibit moderate to low porosity and moderate to high permeability. From the distribution of recoverable oil and gas reserves in African carbonate rocks, there is still a huge exploration space, and the mature theoretical techniques in the genesis and characterization of carbonate reservoirs in China are worthy of further referencing.

There are relatively few summaries and comparative studies on the formation conditions, hydrocarbon accumulation models, and main controlling factors of carbonate oil and gas fields in the South China Sea (SCS), making it difficult to guide oil and gas exploration in similar areas of the SCS. Based on the tectonic background and basement control factors, the carbonate platforms in the SCS are classified into three types: stable, fault-block and inverted. Typical oil and gas fields in each type of platform are selected for dissection to analyze the characteristics of hydrocarbon source- reservoir-cap conditions, hydrocarbon accumulation patterns and main controlling factors. The research suggests that: (1)The source rocks of carbonate reservoirs in the SCS are mostly Oligocene-Miocene coal rocks and coal bearing mudstones form. The reservoirs are mostly composed of Middle-Upper Miocene biogenic reef limestone and calcarenites, with porosity mainly ranging from 20% to 25%, and permeability mainly at the range of (100-200) × 10^-3 μm². The cap rock is Upper Miocene marine mudstone. (2)The three types of platforms exhibit distinct hydrocarbon accumulation models: stable platforms follow a "lower generation, lateral reservoir" model with long-distance migration; fault-block platforms adhere to a "lower generation, lateral reservoir" model with short-distance migration; inverted platforms exhibit a "lower generation, upper reservoir" model with short-distance migration. (3)The three types of carbonate platforms have different potential exploration areas: stable platforms focus on carbonate buildups developed above unconformities or sandstone bodies; fault-block platforms focus on the carbonate buildups on the horst adjacent to the fault depression. For reversed platforms, priority should be given to the carbonate buildups directly developed on the depression, which is also the most important exploration area for carbonate reservoirs in the SCS at present.