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Xie Taijun. The Sedimentary Environment and Organic Matter Distribution of Marine Clastic Source Rocks[J]. Acta Sedimentologica Sinica, 1997, 15(2): 14-18.
Citation: Xie Taijun. The Sedimentary Environment and Organic Matter Distribution of Marine Clastic Source Rocks[J]. Acta Sedimentologica Sinica, 1997, 15(2): 14-18.

The Sedimentary Environment and Organic Matter Distribution of Marine Clastic Source Rocks

  • Received Date: 1996-09-12
  • Publish Date: 1997-04-10
  • There are some differences in sedimentary environments of continental and marine source rocks, thesedimentary model of organic-carbon-rich mudstones was investigated based on the data of marine sourcerocks at hove and abroad. The research result of paleo-oceanography,stratigraphic sequences and oxygenisotopes of plankton Foraminifera indicated that the organic-carbonich sediments in the north Pacificcoust are of similarity in age and paleodimate, according to the data of stratigraphic sequences andgeochemstry,the distribution and cotrolling factor of organic matter were discussed as well.
  • [1] 1 汪品先等.古湖泊学译文集北京:海洋出版社.1991. 27-34.胡见义.黄第藩等.中国陆相石油地质理论基础.北京:石油工业出版社.1991.164-178

    2 Huediger stien, et al. Aecumulation of Organic carbon-Rich Sediments in the late ,Jurassic and Cretaczous Atlantic Oczan-A Synthesis. Chimical Geology. 1986, 56 1-32

    3 Ruediger Stein.Organic-carbon-rich sediments and Paleolnvi-roment, Hesults from Baffin Ray(odp-Leg105) and the up-welling Area off Northwest Africa(0 D P-1 eg 108).AAPGStarlies in Geolog.1990. 3D 41-56

    5 Richard G Miller. A Paleoceanographie Approach to the Kim-meridge clay formation. AAPG studies in Geology#.1990.30 13-26

    6 James C lngle. Origin of Neogene Diatomites Around the North Pacific Rim. Pacific section of SEPM .1981. 159-179.

    7 潘祖荫万晓樵.乐东30-1-1(A)井晚第三纪沉积环境与古生产率.中国海上油气.1994, 8(2): 80-90.
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  • Received:  1996-09-12
  • Published:  1997-04-10

The Sedimentary Environment and Organic Matter Distribution of Marine Clastic Source Rocks

Abstract: There are some differences in sedimentary environments of continental and marine source rocks, thesedimentary model of organic-carbon-rich mudstones was investigated based on the data of marine sourcerocks at hove and abroad. The research result of paleo-oceanography,stratigraphic sequences and oxygenisotopes of plankton Foraminifera indicated that the organic-carbonich sediments in the north Pacificcoust are of similarity in age and paleodimate, according to the data of stratigraphic sequences andgeochemstry,the distribution and cotrolling factor of organic matter were discussed as well.

Xie Taijun. The Sedimentary Environment and Organic Matter Distribution of Marine Clastic Source Rocks[J]. Acta Sedimentologica Sinica, 1997, 15(2): 14-18.
Citation: Xie Taijun. The Sedimentary Environment and Organic Matter Distribution of Marine Clastic Source Rocks[J]. Acta Sedimentologica Sinica, 1997, 15(2): 14-18.
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