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- W2367538219 abstract "Baibao area is located slopes in central and western part of the northern Shanxi in the Ordos Basin,in which a set of delta-lacustrine terrigenous clastic sediments with coal is found in the Late Trias- sic chang4+5 period.According to the trace element analysis of the 28 samples of mudstone from the study area,using the walker method (equivalent boron method),the Adams method and the elemental ratio method (Sr/Ba) conclude that it was the freshwater depositional environment in the period of chang4+5; using iron mineral assemblage method and Fe~(2+)/Fe~(3+) method determine that sedimentary environment was the weak reduction condition at that time;using the method of the combination of elements (Cu,Ba,Ni, etc.) suggest that the sedimentary environment was from lakeshore to shallow lake in depositional period of chang4+5;using the method of the combination of elements(Fe,Mn,Cr,V,Ni,etc.) and the elements ratio (Sr/Ba,Fe~(3+)/Fe~(2+)) inferred that it was humid weather conditions in the chang4+5 depositional peri- od.The inference and analysis from the character of the lacustrine water body and the palaeoclimatology conditions provide corroboration for the causes and distribution of the sand body of the study area in the Late Triassic chang4+5 depositional period." @default.
- W2367538219 created "2016-06-24" @default.
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- W2367538219 date "2008-01-01" @default.
- W2367538219 modified "2023-09-25" @default.
- W2367538219 title "Study on Paleoenvironment of the Late Triassic chang4+5 depositional period of the Baibao area in Ordos Basin" @default.
- W2367538219 hasPublicationYear "2008" @default.
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