The missing upper Carboniferous in the Cimmerian continent: A critical review

The Cimmerian continent is composed of a series of blocks that were attached to the northern margin of Gondwana during the Carboniferous-Permian time, and as a consequence therefore, developed glacial sediments during the Late Paleozoic Ice Age (LPIA). These blocks rifted from Gondwana in the Early...

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Bibliographic Details
Published inEarth-science reviews Vol. 217; p. 103627
Main Authors Wang, Xiang-dong, Hu, Ke-Yi, Shi, Yu-Kun, Chen, Ji-Tao, Yang, Sun-Rong, Ye, Xun-Yan, Li, Xiao-Ming, Song, Ying-Fan, Chen, Bo, Chang, Xiao-Lin, Yao, Le, Zhang, Yi-Chun, Fan, Jun-Xuan, Shen, Shu-Zhong
Format Journal Article
LanguageEnglish
Published Elsevier B.V 01.06.2021
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Online AccessGet full text
ISSN0012-8252
1872-6828
DOI10.1016/j.earscirev.2021.103627

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