Major, trace and platinum-group element geochemistry of the Upper Triassic nonmarine hot shales in the Ordos basin, Central China

•The Upper Triassic Chang 7 hot shales developed under anoxic environment.•Humid paleoclimate was favorable for the deposition of the Chang 7 hot shales.•Tectonics is the major control on the development of the Chang 7 hot shales. The Upper Triassic Chang 7 non-marine hot shales have been proven to...

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Bibliographic Details
Published inApplied geochemistry Vol. 53; pp. 42 - 52
Main Authors Qiu, Xinwei, Liu, Chiyang, Mao, Guangzhou, Deng, Yu, Wang, Feifei, Wang, Jianqiang
Format Journal Article
LanguageEnglish
Published Elsevier Ltd 01.02.2015
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