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- W2352170319 abstract "In early upper Dias,a big northeast—southwest meandering river was formed,which takes the Dachang layer as the basal in the intermont basin in Dachang.The river development is microfacies and the sediments includes: stream-channel conglomerate,point-bar arenyte,vertical-accretion argillite and so on.In this sedimentary layer,the up part contact with the upper Dias Emeishan deposit,the down part contact with Dachang layer or Maoshan formation of Middle Dias.This is the sedimentary affection of Emei Earth mantle surrectic edge." @default.
- W2352170319 created "2016-06-24" @default.
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- W2352170319 date "2008-01-01" @default.
- W2352170319 modified "2023-09-27" @default.
- W2352170319 title "Fluviatile Facies Sedimentary Characters of Early Upper Dias in Dachang of Qinglong,Guizhou and Discussion of the Contacting Relationship with Up and Low Layer" @default.
- W2352170319 hasPublicationYear "2008" @default.
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