The relationship between sedimentary environment and organic matter accumulation in the Niutitang black shale in Zhenyuan, northern Guizhou

被引：0
|
作者：
Xia P. [1 ,2 ]
Fu Y. [1 ,2 ]
Yang Z. [1 ,3 ]
Guo C. [1 ,2 ]
Huang J. [1 ,2 ]
Huang M. [4 ]
机构：
[1] College of Resource and Environmental Engineering, Guizhou University, Guiyang
[2] Key Laboratory of Karst Geological Resources and Environment, Guizhou University, Guiyang
[3] College of Eco-Environmental Engineering, GuizhouMinzu University, Guiyang
[4] 115 Geological Team, Guizhou Bureau of Geological and Mineral Exploration and Development, Guiyang
来源：
Dizhi Xuebao/Acta Geologica Sinica | 2020年 / 94卷 / 03期
关键词：
Black shale; Guizhou; Niutitang Formation; Organic matter; Paleoenvironment;
D O I：
10.19762/j.cnki.dizhixuebao.2020136
中图分类号：
学科分类号：
摘要：
The mineral composition, major and trace elements, carbon and oxygen isotopes were used to analyze the lithofacies type, as well as sedimentary environments of different lithofacies and their relationship with organic matter accumulation in the Niutitang black shale from the well ZX in Zhenyuan County, northern Guizhou area. The results show that the lower member of Niutitang Formation is mainly composed of siliceous shale with TOC of 4.96%~10.1%, and the upper member is mainly composed of mud-rich siliceous shale with TOC of 1.43%~9.04%. Even though both siliceous shale and mud-rich siliceous shale were deposited in a reducing environment, the sedimentary environment of siliceous shale was more reductive than that of the mud-rich siliceous shale. In this study area, oxygen-deficient reducing environment has a stronger influence on organic matter enrichment than hydrothermal action and terrigenous detrital content. © 2020, Science Press. All right reserved.
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页码：947 / 956
页数：9
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共 39 条
  • [1] Algeo T.J., Lyons T.W., Mo-total organic carbon covariation in modern anoxic marine environments: Implications for analysis of paleoredox and paleohydrographic condition, Paleoceanography, 21, 1, pp. 1016-1038, (2006)
  • [2] Algeo T.J., Maynard J.B., Trace-element behavior and redox facies in core shales of Upper Pennsylvanian Kansas-type cyclothems, Chemical Geology, 206, 3-4, pp. 289-318, (2004)
  • [3] Canfield D.E., Factors influencing organic carbon preservation in marine sediments, Chemical Geology, 111, 3, pp. 315-329, (1994)
  • [4] Douthitt C.B., The geochemistry of the stable isotopes of silicon, Geochimica et Cosmochimica Acta, 46, 8, pp. 1449-1458, (1982)
  • [5] Fan D., Ye J., Yang R., Huang Z., The geological events and ore mineralization nearby the Precambrian-Cambrian boundary in Yangtze platform, Acta Sedimentologica Sinica, 5, 3, pp. 81-96, (1987)
  • [6] Guo Q., Shields G.A., Liu C., Strauss H., Zhu M., Pi D., Goldberg T., Yang X., Trace element chemostratigraphy of two Ediacaran-Cambrian successions in South China: Implications for organosedimentary metal enrichment and silicification in the early Cambrian, Palaeogeography Palaeoclimatology Palaeoecology, 254, pp. 194-216, (2007)
  • [7] Han T., Zhu X., Li K., Jiang L., Zhao C., Wang Z., Metal sources for the polymetallic Ni-Mo-PGE mineralization in the black shales of the Lower Cambrian Niutitang Formation, South China, Ore Geology Reviews, 67, pp. 158-169, (2015)
  • [8] He L., Wang Y., Chen D., Wang Q., Wang C., Relationship between sedimentary environment and organic matter accumulation in the black shale of Wufeng-Longmaxi formations in Nanchuan area, Chongqing, Natural Gas Geosciences, 30, 2, pp. 203-218, (2019)
  • [9] Hu J., Ma Y., Wang Z., Liu Y., Gao W., Qian T., Palaeoenvironment and palaeoclimate of the Middle to Late Jurassic revealed by geochemical records in northern margin of Qaidam Basin, Journal of Palaeogeography, 19, 3, pp. 480-490, (2017)
  • [10] Jia Z., Hou D., Sun D., Huang Y., Hydrothermal sedimentary discrimination criteria and its coupling relationship with the source rocks, Natural Gas Geoscience, 27, 6, pp. 1025-1034, (2016)
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