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- W2391244296 abstract "Lithostratigraphic and biostratigraphic studies of the Dewukaxa Formation and Xainza Bed have been came out intensively in the Yungzhug area of Xainza County, North Tibet. The Ordovician-Silurian boundary can be defined precisely in this area.The Dewukaxa Formation and Xainza Bed are entirely marine and consist largely of highly fossiliferous limestone and shale. The Xainza Bed was characterized by the Hirnantia Fauna and the Late Ordorician graptolites. The Dewukaxa Formation was characterized by the abundant Silurian conodonts.But in the base of the Dewukaxa Formation has the Ordovician cono donts. Therefore the Ordovician-Silurian boundary is put at the base of the Dewukaxa Formation. The Dewukaxa Formation conformably cover the Xainza bed." @default.
- W2391244296 created "2016-06-24" @default.
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- W2391244296 date "2005-01-01" @default.
- W2391244296 modified "2023-09-28" @default.
- W2391244296 title "THE ORDOVICIAN—SILURIAN STRATIGRAPHIC STUDY OF THE YUNGZHUG AREA, NORTH TIBET" @default.
- W2391244296 hasPublicationYear "2005" @default.
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