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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Published in | Earth-science reviews Vol. 217; p. 103627 |
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Main Authors | , , , , , , , , , , , , , |
Format | Journal Article |
Language | English |
Published |
Elsevier B.V
01.06.2021
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Subjects | |
Online Access | Get full text |
ISSN | 0012-8252 1872-6828 |
DOI | 10.1016/j.earscirev.2021.103627 |
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