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fault system,Deformation Style and Development Mechanism of the Bachu Uplift,Tarim Basin

Journal of Earth Science 2012年第4期23卷 529-541页

作者：佟殿君张俊霞阳怀忠胡德胜任建业 Key Laboratory of Tectonics and Petroleum Resources of Ministry of Education China University of Geosciences School of Economics and Management China University of Geosciences Beijing Research Institute CNOOC Zhanjiang Branch CNOOC Structral Research Center of Oil&Gas Bearing Basin Ministry of EducationChina University of Geosciences

The Bachu （巴楚） uplift is one of the most active tectonic regions nowadays in the Tarim basin, which is also a faulted block uplift that was intensively active during the Cenozoic. This study was based primarily on the geological structure interpretation of seismic profiles, applying the theories and methods of basin dynamics, structural analysis and tectono-stratigraphic analysis, the geometry and kinematics features of the fault systems in the Bachn uplift were analyzed in detail. Our study shows that each fault belt is mainly characterized by compression and overthrusting, most of the faults initiated and activated during the Mid-Late Himalayan period, and that the general structural styles of the Bachu uplift were basement-involved pop-up thrust faulted block uplift, of which the southern margin was covered by the large-scale decollement fault system. The basement-involved structures widely developed in the higher position of the basement uplift, while decollement fault system developed mainly at the position with gypsum mudstone. The evolution process of Bachu uplift included back-bulge slope of the peripheral foreland basin in Mid-Late Caledonian, forebulge in HercynianYanshanian and the latest compressional faulted block uplift in Mid-Late Himalayan. Meanwhile,the study also suggests that the formation, reconstruction and stabilization of the uplift were controlled by the development and evolution of fault systems clearly. In the early forebulge stage, it was mainly presented as flexural deformation without the developing of thrust faults in the Bachu area; to the late stage, under the influence of violent lateral compression deformation, the faulted block uplift formed finally.

关键词： fault system structural style structural evolution Bachu uplift Tarim basin.

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Features of the fault system and its relationship with migration and accumulation of hydrocarbon in Liaodong Bay

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Petroleum Science 2011年第3期8卷 251-263页

作者： Xu Guosheng Ma Ruolong Gong Deyu Zhou Donghong Li Jianping Guo Yonghua Yuan Haifeng Wu Changrong State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation Chengdu University of Technology Chengdu Sichuan 610059 China Exploration and Development Research Institute Tianjin Branch of CNOOC （China） Co. Ltd. Tanggu Tianjin 300452 China

The fault system of Liaodong Bay developed extensively under the control of the Tanlu fault. The fault system can be grouped into strike-slip faults of grade Ⅰ, trunk faults of grade Ⅱand branch faults （induced faults） of grade Ⅲ respectively based on its developmental scale. The faults of grade Ⅰ and Ⅱwere deep, early and large while the faults of grade Ⅲwere shallow, late and small. The formation, evolution and distribution features played a significant role in controlling the migration of oil and gas in both horizontal and vertical directions. The fluid transfer in the fault system occurred in the process of faulting. The strike-slip and trunk faults moved actively forming predominant pathways for oil and gas migration. The branch faults, with weak activity, generally controlled the development of traps and were beneficial for the accumulation and preservation of oil and gas. The faults of grade Ⅰ and Ⅱ formed the major migration pathways for oil and gas, but their fault activity rates appeared to vary along their strikes. The zones with a relatively low fault activity rate might be favorable for oil and gas accumulation. When the activities of strike-slip, trunk, and branch faults came to a halt, the fault seal behavior had a vitally important effect on the accumulation of oil and gas. The controlling role of the fault over fluid distribution was further analyzed by calculating the fault activity quantitatively.

关键词： Liaodong Bay fault system fault activity rate fault seal behavior migration andaccumulation of oil and gas

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fault system, Diapirism and Oil (Gas) Migrationin the Yinggehai Basin, South China Sea

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Continental Dynamics 2000年第1期 59-66页

作者： YIN Xiulan Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China LI Sitian China University of Geosciences, Wuhan 430074, China YANG Jihai, ZHANG Qiming China Offshore Oil Nahai Weast Corp., Zhangjiang 524057, China

Oil field is closely related to fault systems and diapirs in the Yinggehai basin. Diapirism not only provided a driving force for oil/gas migration, but also opened new faults to provide the oil/gas with migration pathways. Based on the analysis of the fault structures in the basin, the paper discusses tectonic stress fields in the basin and their driving function on fluid. Results show that the stress fields from diapirism determine the fluid migration tendency along the fault zone in the basin.

关键词： fault system diapirism oil/gas migration overpressure fluid

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fault systems and Their Mechanisms of the Formation and Distribution of the Tarim Basin,NW China

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Journal of Earth Science 2014年第1期25卷 169-182页

作者： Liangjie Tang Taizhu Huang Haijun Qiu Guimei Wan Meng Li Yong Yang Daqing Xie Gang Chen State Key Laboratory of Petroleum Resources and Prospecting China University of Petroleum Basin & Reservoir Research Center China University of Petroleum Northwest Oilfield Company SINOPEC Oil and Gas Resources Strategic Research Center

This article aims to analyze the main controlling factors of development, distribution and evolution of the fault systems in the Tarim Basin. Based on the seismic profile interpretation, compre- hensive analysis of the drilling and geologic data, six fault systems maybe recognized in the Tarim Basin, they are the foreland fault system of the South Tianshan Mountain, the northern Tarim uplift fault sys- tem, North Tarim depression fault system, central fault system, Southwest Tarim fault system, and Southeast Tarim fault system. It is indicated that the main differences exist at the development, evolu- tion and distribution of the fault systems in the Tarim Basin. The sub-fault systems can be recognized according to the differences of the fault development and distribution in the interior of the fault system. It is characterized that the multi-level differential development and distribution of the fault systems ex- ist in the Tarim Basin. The fault belt developed in the Paleozoic strata mainly distribute at the pa- leo-uplift and paleo-slope in the interior of the Tarim Basin, and the fault belt occurred in the Meso-Cenozoic beds mainly develop at the peripheral foreland depressions. Zonal and segment differ- ential development and distribution of the fault systems also exist in the Tarim Basin. The formation and distribution of the Tarim fault systems is of complex controlling mechanisms. Poly-phase structural movement and tectonic transition controls the multi-phase differential development and distribution of the fault systems in the Tarim Basin. Multi-level differential development and distribution is controlled by multi-level detachment belt and regional unconformities. Zonal and segment differential develop- ment and distribution of the Tarim fault systems maybe controlled by pre-existed basement structural texture. The major direction of the fault systems in the Tarim Basin is controlled by the later stage basin-mountain coupling.

关键词： fault system differential tectonic movement detachment belt geodynamic mechanism Tarim Basin.

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fault systems and their Control of Deep Gas Accumulations in Xujiaweizi Area

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Acta Geologica Sinica(English Edition) 2012年第6期86卷 1547-1558页

作者： SUN Yonghe KANG Lin BAI Haifeng FU Xiaofei HU Ming Geoscience College Northeast Petroleum University Zhenhua Oil Co.Ltd.

A study of faults and their control of deep gas accumulations has been made on the basis of dividing fault systems in the Xujiaweizi area. The study indicates two sets of fault systems are developed vertically in the Xujiaweizi area, including a lower fault system and an upper fault system. Formed in the period of the Huoshiling Formation to Yingcheng Formation, the lower fault system consists of five fault systems including Xuxi strike-slip extensional fault system, NE-trending extensional fault system, near-EW-trending regulating fault system, Xuzhong strike-slip fault system and Xudong strike-slip fault system. Formed in the period of Qingshankou Formation to Yaojia Formation, the upper fault system was affected mainly by the boundary conditions of the lower fault system, and thus plenty of muiti-directionally distributed dense fault zones were formed in the T2 reflection horizon. The Xuxi fault controlled the formation and distribution of Shahezi coal-measure source rocks, and Xuzhong and Xndong faults controlled the formation and distribution of volcanic reservoirs of Y1 Member and Y3 Member, respectively. In the forming period of the upper fault system, the Xuzhong fault was of successive strong activities and directly connected gas source rock reservoirs and volcanic reservoirs, so it is a strongly-charged direct gas source fault. The volcanic reservoir development zones of good physical properties that may be found near the Xuzhong fault are the favorable target zones for the next exploration of deep gas accumulations in Xujiaweizi area.

关键词： deep gas accumulation fault system gas source fault volcanic reservoir Xujiaweizi

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Sandbox modeling of fault formation and evolution in the Weixinan Sag, Beibuwan Basin, China

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Petroleum Science 2012年第2期9卷 121-128页

作者： Tong Hengmao State Key Laboratory of Petroleum Resource and Prospecting China University of PetroleumBeijing 102249China

fault formation and evolution in the presence of multiple pre-existing weaknesses has not been investigated extensively in rift basins. The fault systems of Weixinan Sag, Beibuwan Basin of China, which is fully covered with high-precision 3-D seismic data and is rich in oil-gas resources, have been successfully reproduced by sandbox modeling in this study with inclusion of multiple pre-existing weaknesses in the experimental model. The basic characteristics of fault formation and evolution revealed by sandbox modeling are as follows. 1） Weakness-reactivation faults and weakness-related faults are formed much earlier than the distant-weakness faults （faults far away from and with little or no relationship to the weakness）. 2） Weakness-reactivation faults and weakness-related faults develop mainly along or parallel to a pre-existing weakness, while distant-weakness faults develop nearly perpendicular to the extension direction. A complicated fault system can be formed in a fixed direction of extension with the existence of multiple pre-existing weaknesses, and the complicated fault system in the Weixinan Sag formed gradually in a nearly N-S direction with multiple pre-existing weaknesses. 3） The increase in the length and number of faults is closely tied to the nature of pre-existing weaknesses. The sandbox model may provide a new clue to detailed fault system research for oil and gas exploration in rift basins.

关键词： fault system rift basin multiple pre-existing weaknesses Weixinan Sag sandbox modeling

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Regional fault systems of Qaidam Basin and Adjacent Orogenic Belts

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Journal of China University of Geosciences 2003年第1期14卷 65-72页

作者： ZhangBingshan TangLiangjie JinZhijun DaiJunsheng ZhangMingli ZhangBingshan QinghaiOilfieldCompany PetroChinaCompanyLtd.Dunhuang841000 Basin&ReservoirResearchCenter UniversityofPetroleumBeijing102249 ResourcesandEnvironmentSchool UniversityofPetroleumDongying257062 QinghaiOilfieldCompany Petro-ChinaCompanyLtd. Dunhuang841000

The purpose of this paper is to analyze the regional fault systems o f Qaidam basin and adjacent orogenic belts. Field investigation and seismic interp retation indicate that five regional fault systems occurred in the Qaidam and ad jacent mountain belts, controlling the development and evolution of the Qaidam b asin. These fault systems are: (1)north Qaidam Qilian Mountain fault system; (2 ) south Qaidam East Kunlun Mountain fault system; (3)Altun strike slip fault s ystem; (4)Elashan strike slip fault system, and (5) Gansen Xiaochaidan fault s ystem. It is indicated that the fault systems controlled the orientation of the Qaidam basin, the formation and distribution of secondary faults within the basi n, the migration of depocenters and the distribution of hydrocarbon accumulation belt.

关键词： fault system thrust fault strike slip fault basin mountain coupl ing Qaidam basin.

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