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- W2393508557 abstract "Based on the analysis of development characteristics of Surennuoer fault and recovering of ancient tectonic stress,vertical open degree of Surennuoer fault of K1d caprock in four tectonic movement periods was studied from the angle between the orientation maximum principal compressive stress and the strike direction of Surennuoer fault.The results show that the vertical open degree of Surennuoer fault is different in different tectonic movement periods,the vertical open degree in southwest of Surennuoer fault is different from that in northeast of Surennuoer fault.By the study of the relation between vertical open degree of Surennuoer fault in different tectonic movement period and the expulsion oil-gas history of K1n1 source rock,it was considered that the third tectonic movement occurring in the later of K2y sedimentation period was rightly the period of a lot of oil-gas expelled from K1n1 source rock.Vertical open of Surennuoer fault are the main transporting pathway of oil-gas migrating from K1n1 source rock to K1n2 reservoirs,and its open degree in K1d1 is not so high so that it is favorable for oil-gas to accumulate and preserve in K1n2.This is the important cause that there are a lot of hydrocarbon to accumulate in K1n2.But vertical open degree in southwest of Surennuoer fault is lower than that in northeast of Surennuoer fault in this tectonic movement period.The oil-gas accumulation and preservation conditions in southwest of Surennuoer fault are better than that in northeast of Surennuoer fault.This is the important reason why there are more industrial oil-gas accumulations in southwest of Surennuoer fault than in southeast of Surennuoer fault." @default.
- W2393508557 created "2016-06-24" @default.
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- W2393508557 date "2008-01-01" @default.
- W2393508557 modified "2023-09-26" @default.
- W2393508557 title "Vertical open degree of Surennuoer fault in different tectonic movement periods and its relation with oil and gas vergency" @default.
- W2393508557 hasPublicationYear "2008" @default.
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