|
|
|
题名
|
作者
|
年代
|
出处
|
被引量
|
| 1 | Control of differential tectonic evolution on petroleum occurrence in Bohai Bay Basin显示文摘The Bohai Bay Basin(BBB)is the most petroliferous Cenozoic basin in the east of China.It consists of seven depressions.Each depression has been subjected to different stress states and then has experienced varying faulting processes since the Neogene,especially during the Neotectonism(from the Pliocene to the present).On the basis of the investigation of fault patterns,fault densities and fault activity rates(FARs)for each depression,this paper demonstrates the discrepancy of faulting development and evolution across the BBB.The dynamic mechanism for the differences in faulting is also discussed by the analysis of the regional stress state.The Bozhong Depression is just situated in the transtensional zone induced by the two active strike-slip faults,namely Yingkou-Weifang and Beijing-Penglai.In this depression,the major faults which cut through the Paleogene or the Cenozoic have had higher than 10 m/Ma FARs since the Neogene,and the highest FARs have reached or exceeded 25 m/Ma during the Neotectonism.As a result,most of the petroleum has migrated along these major faults and accumulated within the Neogene.In contrast,in the other depressions of the BBB away from the Bozhong Depression,the FARs of the major faults were decreased to lower than 10 m/Ma since the Neogene,and tended to be zero during the Neotectonism.Therefore,the major faults could not serve as vertical conduits for petroleum migration,and the petroleum was entrapped in the Paleogene.Consequently,the faulting since the Neogene,especially during the Neotectonism,controlled the petroleum richness in vertical strata. | TENG ChangYu ZOU HuaYao HAO Fang | 2014 | Science China Earth Sciences2014，57，5： | 13 |
| 2 | Source Rocks for the Giant Puguang Gas Field,Sichuan Basin:Implication for Petroleum Exploration in Marine Sequences in South China显示文摘摘要:详细地球化学研究被进行在巨大的 Puguang 煤气的领域里调查稳固的沥青和烃气体的起源。稳固的沥青的二种类型被认出:低硫在在 Xujiahe 形成和高硫的沙岩水库的沥青满足的满意的、低反射(LSLR ) 固体,高反射(HSHR ) 固体在在更低的三叠纪的 Feixianguan 和上面的二叠的 Changxing 形成的碳酸盐水库的沥青。在上面的三叠纪的 Xujiahe 形成的稳固的沥青与摘录相关很好从上面对在同位素的作文的侏罗记 nonmarine 来源岩石三叠纪浸透并且芳香的部分和 biomarker 分发。在 Feixianguan 和 Changxing 形成的稳固的沥青与摘录从显然不同寒武纪并且志留纪岩石但是在同位素的作文两个都从上面的二叠的来源岩石与摘录显示合理关联浸透并且芳香的部分并且在 biomarker 分发,建议二叠特别上面的二叠的 Longtan 形成是在在在 th 的 Feixianguan 和 Changxing 形成的碳酸盐水库的稳固的沥青的主要来源天然气的化学、同位素的作文显示烃气体的多数从生存于富有腐殖质的有机物发源并且是积累的油的热裂开的产品。这研究显示生存于富有腐殖质的有机物统治的那来源岩石存在在上面二叠并且做了主要贡献到巨大的 Puguang 煤气的地,它在华南在海洋的序列为石油探索有重要牵连。 | ZOU Huayao HAO Fang ZHU Yangming GUO Tonglou CAI Xunyu LI Pingping ZHANG Xuefeng | 2008 | Acta Geologica Sinica(English Edition)2008，82，3： | 11 |
| 3 | Preferential petroleum migration pathways and prediction of petroleum occurrence in sedimentary basins:A review显示文摘The aim of this paper is to review the major points of contention concerning secondary petroleum migration,to discuss the nature and primary controls of the positions of petroleum migration pathways in sedimentary basins,and to illustrate the importance of preferential petroleum migration pathways for the formation of large oil/gas fi elds away from generative kitchens. There is competition between the driving force(buoyancy) and the restraining force(capillary pressure controlled largely by permeability contrast) in controlling the positions of petroleum migration pathways in heterogeneous carrier beds. At a large scale,there is a critical angle of dip of the carrier beds which determines the relative importance of structural morphology or permeability contrasts in controlling the positions of petroleum migration pathways in heterogeneous carrier beds. Maximum-driving-force-controlled migration pathways occur in carrier beds with an angle of dip greater than the critical dip and the positions of petroleum migration pathways are controlled mainly by the morphology of the sealing surfaces. Minimum-restraining-force-determined migration pathways occur in carrier beds with an angle of dip smaller than the critical angle where permeability contrasts would exert a more important influence on the positions of petroleum migration pathways. Preferential petroleum migration pathways(PPMP) ,defi ned as very restricted portions of carrier-beds that focus or concentrate petroleum from a large area of the generative kitchen,determine the distribution of oil and gas in sedimentary basins. The focusing of petroleum originating from a large area of the generative kitchens into restricted channels seems to be essential not only for long-range petroleum migration in hydrostatic conditions,but also for the formation of large oil or gas fi elds. Regions may miss out on petroleum migration because of its three-dimensional behavior,and two-dimensional migration modeling may be misleading in predicting petroleum occurrences in certain circumstances. | Hao Fang Zou Huayao Gong Zaisheng | 2010 | Petroleum Science2010，7，1： | 8 |
| 4 | Late-stage rapid accumulation of the PL19-3 giant oilfield in an active fault zone during Neotectonism in the Bozhong depression,Bohai Bay显示文摘Late-stage is defined here as the period when Neotectonism occurred since 5.1 Ma. Most petroliferous basins in China lie in the areas where Neotectonism occurred intensively. In recent years, Chinese petroleum geologists have paid much attention to late-stage petroleum accumulation. The PL19-3 giant oilfield is situated where faulting activities occurred violently during Neotectonism. To understand the mechanism of lat-stage rapid accumulation, we discussed the most important aspects responsible for the formation of the giant oilfield, including oil generation, active oil-source rock occurrence, fault activity and fault conduits, late-stage rapid oil injection as well as the distinguishing indicators. This study shows that: (1) sufficient oil was supplied to the PL19-3 field since 5.1 Ma because the PL19-3 structure was surrounded by four sags in which three intervals of high-quality source rocks remained active during Neotectonism; (2) densely distributed faults and high porosity/permeability sandstone carrier beds comprised the effective conduit system for oil migration and injection; (3) oil migrated along the faults and charged the PL19-3 structure rapidly by means of seismic pumping which was triggered by frequent earthquakes during Neotetonism. It is documented that elevated reservoir temperature, abnormal geothermal gradients and abnormally high homogenization temperatures of the fluid inclusions are the indicators for late-stage rapid oil accumulation. | ZOU HuaYao GONG ZaiSheng TENG ChangYu ZHUANG XinBin | 2011 | Science China Earth Sciences2011，54，3： | 8 |
| 5 | Process and mechanism for oil and gas accumulation, adjustment and reconstruction in Puguang Gas Field, Northeast Sichuan Basin, China显示文摘With the discoveries of a series of large gas fields in the northeast of Sichuan Basin, such as Puguang and Longgang gas fields, the formation mechanism of the gas reservoir containing high H2S in the ancient marine carbonate formation in superposition-basin becomes a hot topic in the field of petroleum geology. Based on the structure inversion, numerical simulation, and geochemical research, we show at least two intervals of fluid transfer in Puguang paleo-oil reservoir, one in the forepart of late Indo-Chinese epoch to early Yanshan epoch and the other in the metaphase of early Yanshan epoch. Oil and gas accumulation occurred at Puguang structure through Puguang-Dongyuezhai faults and dolomite beds in reef and shoal facies in Changxing Formation (P2ch) - Feixianguan Formation (T1f) in the northwest and southwest directions along three main migration pathways, to form Puguang paleo-oil reservoir. Since crude oil is pyrolysised in the early stage of middle Yanshan epoch, Puguang gas reservoir has experienced fluid adjusting process controlled by tectonic movement and geochemical reconstruction process controlled by thermochemical sulfate reduction (TSR). Middle Yan-shan epoch is the main period during which the Puguang gas reservoir experienced the geochemical reaction of TSR. On one hand, TSR can recreate the fluid in gas reservoir, which makes the gas drying index larger and carbon isotope heavier. On the other hand, the reciprocity between fluid regarding TSR (hydrocarbon, H2S, and water) and reservoir rock induces erosion of the reservoir rocks and anhydrite alteration, which improves reservoir petrophysical properties. Superimposed by later tectonic movement, the fluid in Puguang reservoir has twice experienced adjustment, one in the late Yanshan epoch to the early Himalayan epoch and the other time in late Himalayan epoch, after which Puguang gas reservoir is finally developed. | DU ChunGuo HAO Fang ZOU HuaYao ZHU YangMing CAI XunYu WANG CunWu | 2009 | Science China Earth Sciences2009，52，9： | 6 |
| 6 | Thermal evolution and applications of aromatic hydrocarbons in highly mature coal-bearing source rocks of the Upper Triassic Xujiahe Formation in the northern Sichuan Basin显示文摘Based on the GC-MS analytical data of aromatic fractions of over forty highly mature coal-bearing source rock samples collected from the Upper Triassic Xujiahe Formation in the northern Sichuan Basin, the thermal evolution of aromatic hydrocarbons during late-mature to over-mature stage(Ro=1.13%–2.85%) was characterized, and aromatic indicators suitable for recognizing the organic source and sedimentary environment of high maturity source rocks were discussed. The results indicated that the concentrations of low carbon-cycle naphthalene as well phenanthrene series reduce gradually with increasing Ro at the highly mature levels. However, some high-cyclic components such as chrysene, benzofluoranthene, and benzo[e]pyrene are relatively enriched, in companying an enhancement of parent aromatic compounds. The variations are attributed to thermal cracking and polymerization reactions due to continuous dehydrogenation under enhanced burial temperature. As thermal maturity rises, MPI1(Methylphenanthrene Index) values display a two-modal varying trend, namely, increasing when Ro is below 1.80% and decreasing above 1.8% Ro. The relationships between Ro and MPI1 are Ro=0.98MPI1+0.37 for Ro<1.80% and Ro=?0.90MPI1+3.02 at Ro>1.8%, being different from the previous research. The amount of dibenzofurans declines sharply at Ro higher than 1.1%, leading to a significant change of relative composition among dibenzothiophenes, dibenzofurans and fluorenes(referred as three-fluorenes series composition). Thus, this parameter appears to be unsuitable for identifying the sedimentary environment of the highly matured source rocks. 4-/1-MDBT(methyldibenzothiophene) ratio could be served as an effective indicator for organic facies, and can distinguish coals from mudstones at over-maturity in this case. The ratios of 2,6-/2,10-DMP(dimethylphenanthrene) and 1,7-/1,9-DMP and relative abundance of triaromatic steroids in these highly mature rocks could be considered as biological source parameters for relative input of terrigenous versus aquatic organic matter. | LI Ying ZHU YangMing HAO Fang ZOU HuaYao GUO TongLou | 2015 | Science China Earth Sciences2015，58，11： | 4 |
| 7 | Accumulation Mechanisms and Evolution History of the Giant Puguang Gas Field,Sichuan Basin,China显示文摘稳固的沥青在 Puguang 煤气的地里在整个碳酸盐水库被发现,最大的煤气的地到目前为止在中国在海洋的碳酸盐发现了,证实 Puguang 煤气的地从一座 paleo 油水库演变。液体水管系统在这域里的集中的油累积的时候被重建,并且石油移植小径用一个 3-D 模型被建模并且由 geochemical 参数跟踪了。向前建模并且倒置跟踪与对方一起与一致,两个显示油在 Puguang-Dongyuezhai 结构积累了从一个生产厨房发源到 Puguang 气体地的西北。生存于富有腐殖质的有机物在东北四川盆,是垂直地近来源的岩石和旁边地在生产附近的厨房的液体水管系统的发展,并且集中油统治的器官富人的上面的二叠的来源岩石的免职从生产厨房的一个大区域发源,是为巨大的 Puguang 煤气的地从演变的巨大的paleo油水库的形成的三个要求。Puguang 煤气的地经历了三阶段的进化。累积以后的进程,特别在 hydrocarbon-water-rock 系统的器官无机的相互作用,深刻地不仅改变了石油液体的作文和特征,而且显然在水库改变了物理化学的条件并且导致了碳酸盐矿物质的复杂降水和答案。 | HAO Fang GUO Tonglou DU Chunguo ZOU Huayao CAI Xunyu ZHU Yangming LI Pingping WANG Chunwu ZHANG Yuanchun | 2009 | Acta Geologica Sinica(English Edition)2009，83，1： | 4 |
| 8 | Rapid hydrocarbon accumulation mechanism in later period in Kelasu thrust belt in Kuqa depression显示文摘Based on the analyses of generation, migration and accumulation of oil and gas in the structures of Kela 1, Kela 2 and Kela 3 in Kasangtuokai anticlinal belt using a series of geological and geochemical evidence, this paper proposes that the rapid rate of hydrocarbon generation, main drain path for over-pressured fluid flow and converging conduit system are indispensable conditions for the rapid, late-stage gas accumulation in the Kelasu thrust belt in the Kuqa depression. Due to structural over-lapping and the resultant rapid burial, the maturity of the source rocks had been increased rapidly from 1.3 to 2.5% Ro within 2.3 Ma, with an average rate of Ro increase up to 0.539% Ro/Ma. The rapid matura-tion of the source rocks had provided sufficient gases for late-stage gas accumulation. The kelasu structural belt has a variety of faults, but only the fault that related with fault propagation fold and cut through the gypsiferous mudstone cap could act as the main path for overpressured fluid release and then for fast gas accumulation in low fluid potential area. All the evidence from surface structure map, seismic profile explanation, authigenic kaolinite and reservoir property demonstrates that the main drain path related with faults for overpressured fluid and the converging conduit system are the key point for the formation of the giant Kela 2 gas field. By contrast, the Kela 1 and Kela 3 structures lo-cated on both sides of Kela 2 structure, are not favourable for gas accumulation due to lacking con-verging conduit system. | ZOU HuaYao WANG HongJun HAO Fang LIU GuangDi ZHANG BaiQiao | 2007 | Science China Earth Sciences2007，50，8： | 3 |
| 9 | Origin of Taiwan Canyon and its effects on deepwater sediment显示文摘The continental slope of the Taiwan Shoal, which has cultivated numerous submarine canyons, is located in a passive continental margin environment. However, the trend of the Taiwan Canyon, with its 45° intersection angle, is obviously different from that of the erosion valley downward along the continental slope. A distinct break is present in the lower segment of the Taiwan Canyon, which then extends from west to east parallel to the continental slope until finally joining the Manila Trench. By utilizing multiple-beam water depth data, high-resolution seismic data, and sediment cores, this study describes the topographic characteristics of the Taiwan Canyon and provides a preliminary discussion on the origin of the Taiwan Canyon and its effect on deepwater sediment. The terrain, landform, and sediment of the Taiwan Canyon exhibit segmentation characteristics. The upper segment is characterized primarily by erosion, downward cutting with a V shape, and wide development of sliding, slumping, and other gravity flow types. The middle segment is characterized mostly by U-shaped erosion-sedimentation transition and development of an inner levee. The lower segment is characterized primarily by sedimentation and development of a sediment wave. The bottom current has a significant reworking effect on the interior sediments of the canyon and forms reworked sands. The formation and evolution of the Taiwan Canyon is closely related to sediment supply, gravity sliding(slumping), faulting activities, and submarine impaling. Given the sufficient terrigenous clastic supply, the sediments along the continental shelf edge continuously proceed seaward; gliding and slumping in the front edge provide driving forces for the formation of the canyon. Faulting activities result in stratum crushing, and the gravity flow takes priority in eroding the relatively fragile stratum. Thus, the direction of the extension of the canyon crosses the surrounding erosion valley obliquely. Seamounts are formed through submarine impaling. Owing to seamount blocking, the lower segment of the canyon is turned toward the east–west direction. Large amounts of sediments overflow at the turning, forming sediment waves. | XU Shang WANG YingMin PENG XueChao ZOU HuaYao QIU Yan GONG ChengLin ZHUO HaiTeng | 2014 | Science China Earth Sciences2014，57，11： | 2 |
| 10 | Diagenesis and Restructuring Mechanism of Oil and Gas Reservoir in the Marine Carbonate Formation,Northeastern Sichuan:A Case Study of the Puguang Gas Reservoir显示文摘Based on the technology of balanced cross-section and physical simulation experiments associated with natural gas geochemical characteristic analyses, core and thin section observations, it has been proven that the Puguang gas reservoir has experienced two periods of diagenesis and restructuring since the Late Indo-Chinese epoch. One is the fluid transfer controlled by the tectonic movement and the other is geochemical reconstruction controlled by thermochemical sulfate reduction (TSR). The middle Yanshan epoch was the main period that the Puguang gas reservoir experienced the geochemical reaction of TSR. TSR can recreate the fluid in the gas reservoir, which makes the gas drying index higher and carbon isotope heavier because C2+ (ethane and heavy hydrocarbon) and 12C (carbon 12 isotope) is first consumed relative to CH4 and 13C (carbon 13 isotope). However, the reciprocity between fluid regarding TSR (hydrocarbon, sulfureted hydrogen (H2S) , and water) and reservoir rock results in reservoir rock erosion and anhydrite alteration, which increases porosity in reservoir, thereby improving the petrophysical properties. Superimposed by later tectonic movement, the fluid in Puguang reservoir has twice experienced adjustment, one in the late Yanshan epoch to the early Himalayan epoch and the other time in late Himalayan epoch, after which Puguang gas reservoir is finally developed. | DU Chunguo WANG Jianjun ZOU Huayao ZHU Yangming WANG Cunwu | 2009 | Acta Geologica Sinica(English Edition)2009，83，6： | 2 |
| 11 | The fate of CO 2 derived from thermochemical sulfate reduction (TSR) and effect of TSR on carbonate porosity and permeability, Sichuan Basin, China显示文摘 | Fang Hao Xuefeng Zhang Cunwu Wang Pingping Li Tonglou Guo Huayao Zou Yangming Zhu Jianzhang Liu Zhongxian Cai | 2014 | Earth-Science Reviews2014，，： | 1 |
| 12 | Jurassic oils in the central Sichuan basin, southwest China: Unusual biomarker distribution and possible origin 显示文摘 | Zhu Yangming Hao Fang Zou Huayao | 2007 | Organic Geochemistry2007，38，： | 1 |
| 13 | Mechanisms of shale gas storage:Implications for shale gas exploration in China显示文摘 | Hao Fang Zou Huayao Lu Yongchao | 2013 | AAPG Bulletin2013，97，8： | 1 |
| 14 | Cause of shale gas geochemical anomalies and mechanisms for gas enrichment and depletion in high-maturity shales显示文摘 | Fang Hao Huayao Zou | 2013 | Marine and Petroleum Geology2013，，： | 1 |
| 15 | The overpressure differently and levelly retard the organic matter evolution显示文摘 | Hao Fang Jiang Jianqun Zou huayao | 2004 | Science in China:Series D2004，34，5： | 1 |
| 16 | The overpressure differently and levelly retard the organic matter evolution 显示文摘 | Hao Fang Jiang jianqun Zou huayao | 2004 | Science in China( D )2004，34，5： | 1 |
| 17 | Evolution of overpressured systems in sedimentary basins and conditions for deep oil/gas accumulation显示文摘 | HAO Fang ZOU Huayao NI Jianhua | 2002 | Earth Science2002，27，5： | 1 |
| 18 | Mechanisms of shale gas storage:Implications for shale gas exploration in China显示文摘 | Hao Fang Zou Huayao Lu Yongchao | | 0，，8： | 1 |
| 19 | Petroleum migration and accumulation in the Bozhong sub-basin, Bohai Bay basin, China: Significance of preferential petroleum migration pathways (PPMP) for the formation of large oilfields in lacustrine fault basins显示文摘 | Hao Fang Zou Huayao Gong Zaisheng | 2007 | Marine and Petroleum Geology2007，24，1： | 1 |
| 20 | Mechanisms of petroleum accumulation in the Bozhong sub-basin, Bohai Bay Basin, China. Part 1: Origin and occurrence of crude oils显示文摘 | Fang Hao Xinhuai Zhou Yangming Zhu Huayao Zou Xiaohuan Bao Qingying Kong | 2008 | Marine and Petroleum Geology2008，，8： | 1 |
您所在的机构暂未开通此部分的功能，请联系管理员