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- W2352090968 abstract "Based on the mechanics analysis of fault formation,a systematic study of the fault styles of the deep part of the western Huimin depression,including the basin basement,the Kongdian group(Ek),and the fourth member of the Shahejie group(Es4),was carried out.The main features of faults within the depression,including their distribution,timing of activity,and their influence on the Paleogene basin that evolved into the western Huimin depression,were constrained by interpretations of horizontal slices and cross-sections of 3D seismic data,and the analysis of regional tectonic maps.Also the cause of fracture formation,the nature of the Paleogene prototype basin,and the control of faulting on the formation of oil-gas reservoirs were considered.The results reveal two types of deep fractures in the western Huimin depression,based on tectonic style: strike-slip and extensional.The formation of basement faults was related to sinistral strike-slip movement along the Tan-Lu fault and counter-clockwise rotation of the Luxi uplift during the late Yanshanian,and the fault style during Ek-Es4 sedimentation was closely related to NNW-SSE extension and dextral strike-slip movement upon large deep-level faults(e.g.,the Tan-Lu fault).The distribution and sedimentary characteristics of deep-level faults indicate that the formation of the Paleogene precursor basin in the western Huimin depression was closely related to strike-slip faulting,suggesting the precursor basin was a transtensional structure rather than a purely extensional structure.The style of deep-level faults controlled not only the internal structures of the basin,but also the distribution of sandy layers,which provided a pathway of oil and gas migrating toward areas with shallowly dipping beds,thereby ultimately controlled the formation of oil and gas reservoirs." @default.
- W2352090968 created "2016-06-24" @default.
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- W2352090968 date "2011-01-01" @default.
- W2352090968 modified "2023-09-25" @default.
- W2352090968 title "Style of deep faulting and its control on the Paleogene basin evolved into the western Huimin depression,Eastern China" @default.
- W2352090968 hasPublicationYear "2011" @default.
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