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- W2382078151 abstract "Recently,a new paleo-weathering crust occurred at the top of Carboniferous and Permian strata and Xiaochaka Formation,was discovered in the North Qiangtang depression,central uplift and the South Qiangtang depression during field investigation of petroleum geology,indicating a regional distribution.New geologic survey indicates that the era of weathering and erosion are various in different regions.During the Late Permian,most part of the South Qiangtang and central uplift regions was uplifted into a land and subjected to the weathering and erosion,and then a paleo-weathering crust was formed widely at the top of the Longge and Lugu Formation.By the Late Triassic,most part of the North Qiangtang region was also uplifted into a land and subjected to the weathering and erosion,and then a large weathering and erosion region,including the North Qiangtang depression,central uplift and the South Qiangtang depression,was formed.After a short erosion process(especially for the Xiaochaka Formation),these paleo-weathering crusts were overlapped by the Nadi Kangri volcanic-volcaniclastic rocks and corresponding sediments.The discovery of large-scale paleo-weathering crust is important for assessing petroleum geological conditions in the Qiangtang basin and the overall significance of basin evolution." @default.
- W2382078151 created "2016-06-24" @default.
- W2382078151 creator A5079743933 @default.
- W2382078151 date "2009-01-01" @default.
- W2382078151 modified "2023-09-23" @default.
- W2382078151 title "Discovery of the large-scale paleo-weathering crust in the Qiangtang basin,northern Tibet, China and its significance" @default.
- W2382078151 hasPublicationYear "2009" @default.
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