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- W2354852752 abstract "Ediacaran system in Guizhou Province is made up of Doushantuo Formation and Dengying Formation,in which Doushantuo Formation is mainly composed of siliceous rock,and Dengying Formation is mainly marked by micritic dolomite.On basis of sequence-stratigraphic division for some typical sections,sequence-stratigraphic framework for Ediacaran system in southeastern part of Guizhou Province can be established.The stratigraphic succession from Doushantuo Formation to Dengying Formation constitute an upward shoaling sedimentary succession,and this succession make up one second-order sequence that can be further divided into 5 third-order sequence.Importantly,the similarity of succession of sedimentary facies between second-order and third-order sequences reflects basic feature,i.e.cycle within cycle.Furthermore,an important phenomenon that dolomites in shallow platform do not change into limestone in deep-water basin within Dengying Formation reflects an important sedimentary feature,i.e.this set of dolomits may be resulted from primary precipitation that is same as formation of cap dolomite in bottom of Doushantuo Formation and may represent continuation of the extreme greenhouse effect in Late Precambrian." @default.
- W2354852752 created "2016-06-24" @default.
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- W2354852752 date "2010-01-01" @default.
- W2354852752 modified "2023-09-23" @default.
- W2354852752 title "Sequence-Stratigraphic Framework for the Ediacaran in the Southeastern Part of Guizhou Province" @default.
- W2354852752 hasPublicationYear "2010" @default.
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