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Sequence Stratigraphy and Depositional Environments of the Kuche Depression[J]. Acta Sedimentologica Sinica, 2002, 20(3): 400-407.
Citation: Sequence Stratigraphy and Depositional Environments of the Kuche Depression[J]. Acta Sedimentologica Sinica, 2002, 20(3): 400-407.

Sequence Stratigraphy and Depositional Environments of the Kuche Depression

  • Received Date: 2001-09-17
  • Based on the analysis of outcrops,well logs and high resolution seismic reflection data,this paper tries to interpret the depositional enVironment and the seCuence stratigraphy of Jurassic in Kuche depression. The results show that the Kuche basin is a non-symmetry depression basin,of which the proVenance is from the north. There are 13 third seCuences and 3 seCuence beds,which are t he results of 3 cycles. The large lake transgression is the middle upper of Yangxia For mation,which is consistent to the hot climate. The enVironment is the braided riVer,meandering riVer- delta,and delta and shallowlake,with the ephemeral sea transgression. The source rock is well distributed in the ephemeral sea transgression and the large lake transgression in the middle Jurassic. the reservoir distribution is the key factor to forming oil and gas accumulation.the river reservoir heterogeneity is controlled by the terrestrial environment,although t here are the Well distri bution of the sandbody and great reservoir thickness.
  • [1] 邓宏文.美国层序地层学研究的新学派--高分辨率层序地层学[J].石油与天然气地质. 1995,16(2):89~97[Deng H W.A new school of thought in sequence stratigraphic studies in U. S.:High-resolution sequence stratigraphy[J].Oil and Gas Geology.1995,16(2):89~97]
    [2] 薛良清.层序地层学在湖相盆地中的应用探讨[J].石油勘探与开发, 1996,17(6):29~34[Xue L Q.Application of sequence stratigraphy to the lacustrine basins[J].Petroleum Exploration and Development,1990,17(6):29~34]
    [3] 李思田主编.含能源盆地沉积体系[M]. 武汉:中国地质大学出版社,1996[Li S T.Depositional systems in energy resources-bearing basins[M].Wu Han:China University of Geosciences Press,1996]
    [4] 张希明.塔里木盆地北部中、新生代陆相沉积盆地层序特征[J].石油试验地质,1997,19(1):5~11[Zhang X M.Sequence stratigraphic characterisics of Mesozoic and Cenozoic continental sedimentafy basins in north Tarim basin[J].Experimental Petroleum Geology,1997,19(1):5~11]
    [5] 顾家裕主编.塔里木盆地沉积层序特征及其演化[M].北京:石油工业出版社, 1996.36~72[Gu J Y.Sedimentary sequence stratigeaphic characteristics and evolution of Tarim basin[M].Beijing:Petroleum Industry Press,1996.36~72]
    [6] Pinous O V, Sahagian D L, Shurygin B N, Nikitenko B L. High-resolution sequence stratigraphic analysis and sea-level interpretation of the Middle and Upper Jurassic strata of the Nyurolskaya Depression and vicinity (southwestern West Siberia, Russia) [J]. Marine and Petroleum Geology,1999, 16(3):245~257
    [7] Potocki D. Controls on the stratigraphic distribution of lithotypes, and reservoir quality forecasting, for sandstones in the Western Canada foreland basin[J]. CSPG Reservoir,1995, 22(5): 2~3
    [8] Kuandykov B M, Nazhmetdinov A S, Sapozhnikov R B. Structure of the deeply subsided sediments of the Aryskum Downwarp of the South Turgay Depression based on seismo-stratigraphic data[J]. Petroleum Geology,1993,27(7~8):262~266
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  • Received:  2001-09-17

Sequence Stratigraphy and Depositional Environments of the Kuche Depression

Abstract: Based on the analysis of outcrops,well logs and high resolution seismic reflection data,this paper tries to interpret the depositional enVironment and the seCuence stratigraphy of Jurassic in Kuche depression. The results show that the Kuche basin is a non-symmetry depression basin,of which the proVenance is from the north. There are 13 third seCuences and 3 seCuence beds,which are t he results of 3 cycles. The large lake transgression is the middle upper of Yangxia For mation,which is consistent to the hot climate. The enVironment is the braided riVer,meandering riVer- delta,and delta and shallowlake,with the ephemeral sea transgression. The source rock is well distributed in the ephemeral sea transgression and the large lake transgression in the middle Jurassic. the reservoir distribution is the key factor to forming oil and gas accumulation.the river reservoir heterogeneity is controlled by the terrestrial environment,although t here are the Well distri bution of the sandbody and great reservoir thickness.

Sequence Stratigraphy and Depositional Environments of the Kuche Depression[J]. Acta Sedimentologica Sinica, 2002, 20(3): 400-407.
Citation: Sequence Stratigraphy and Depositional Environments of the Kuche Depression[J]. Acta Sedimentologica Sinica, 2002, 20(3): 400-407.
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