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- W2364879904 abstract "The black shale of Niutitang formation in the studied area mainly developed in the shelf sedimentary environment. we focus on the section-Yonghe profile in Weng’an,Guizhou, and think the black shale of Niutitang formation is divided into transgressive systems tract (TST) and high system tract (HST) on the sedimentary characteristics on the basis of research, combined with the well profile, black shale distribution, geochemical elements analysis, on the northern Guizhou sedimentary characteristics were analyzed. The Niutitang Formation overlying as Sinian grey dolomite, Niutitang Formation deposited in the bottom of a set of black siliceous rocks, to black mudstones, upper muddy siltstone, sandstone. Overall appears up graded to attenuate after coarse features; plane, Guizhou north in the lower Cambrian Niutitang Formation depositional environment is shallow sea shelf sedimentary depositional system types, mainly for shallow continental shelf and deep shelf. To the southeast, water depth increasing,black shale thickness thickened, black shale color burn. Niutitang Formation depositional environment controls the development of the black shale and maturity of organic matter, and the preservation of organic matter. In northern Guizhou Niutitang Formation black shale has the characteristics of wide, large thickness, color pure, rich in organic matter and siliceous shale gas content is higher, is a favorable area for exploration of shale gas." @default.
- W2364879904 created "2016-06-24" @default.
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- W2364879904 date "2011-01-01" @default.
- W2364879904 modified "2023-10-02" @default.
- W2364879904 title "Characteristics of black shale, sedimentary evolution and shale gas exploration prospect of shelf face taking Weng'an Yonghe profile Niutitang group as an example" @default.
- W2364879904 hasPublicationYear "2011" @default.
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