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- W3142777234 abstract "The Hebukehe Formation and related strata in Wulankeshun region,previously assigned to the Lower Carboniferous,are here redefined to the Zhulumute Formation.Our studies show that the Zhulumute Formation is separated from the underlying Silurian volcaniclastic strata by an angular unconformity, but it is conformably overlain by the Late Devonian-Early Carboniferous Hongguleleng Formation.The newly founded fossil plants(Leptophloeum rhombicum)and conodonts(Icriodus-Polygnathus assemblage)indicate that geological age of the Zhulumute Formation is Late Devonian.Facies indicators show that the sedimentary environment of the Zhulumute Formation gradually evolved from a braided fluvial system to a meandering fluvial system.The flow direction was toward NEE.The new data reported are significant for the stratigraphic subdivision and correlation,as well as paleoenvironmental investigation,of the Upper Paleozoic in western Junggar." @default.
- W3142777234 created "2021-04-13" @default.
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- W3142777234 date "2014-01-01" @default.
- W3142777234 modified "2023-09-23" @default.
- W3142777234 title "NEW KNOWLEDGE ABOUT THE LATE DEVONIAN ZHULUMUTE FORMATION IN THE WULANKESHUN REGION,WESTERN JUNGGAR" @default.
- W3142777234 hasPublicationYear "2014" @default.
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