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- W2373153744 abstract "The tectonic framework of the eastern Tianshan has been one of the controversial issues in the geological community for a long time. During 1∶50000 regional geological and mineral survey,some conodonts fossils such as of Streptognathodus suberectus,Idiognathoides sinuate et al. are discoveried in limestone of the Kumutag sand-rigde located in the north of kangguurtag deep fault. The age of the stratum within these conodonts fossils can be confirmed in the Upper Carboniferous Dalaan Stage. And it belongs to the Karlik minor strata area, which has the feature of back-arc basin formation. The north boundary of the kangguurtag deep fault zone has been limited by the distributing of the Dikan’er formation, it has important value in regional stratigraphic division and correlation and the confirmation of tectonic boundary." @default.
- W2373153744 created "2016-06-24" @default.
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- W2373153744 date "2007-01-01" @default.
- W2373153744 modified "2023-09-23" @default.
- W2373153744 title "THE DISCOVERY OF CONODONTS FOSSILS IN CARBONIFEROUS OF KUMUTAG AREA IN THE EASTERN TIANSHAN AND ITS SIGNIFICANCE" @default.
- W2373153744 hasPublicationYear "2007" @default.
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