Late Cambrian climate change recorded by a shift from an arid carbonate platform to a storm‐dominated cool‐water platform at the Gondwana margin (Alborz Zone, Iran)-Reference-Cited by-同舟云学术

Late Cambrian climate change recorded by a shift from an arid carbonate platform to a storm‐dominated cool‐water platform at the Gondwana margin (Alborz Zone, Iran)

Published:2022-11-03 Issue:2 Volume:58 Page:795-824
ISSN:0072-1050
Container-title:Geological Journal
language:en
Short-container-title:Geological Journal

Author:

Daraei Mehdi¹^ORCID,Bayet‐Goll Aram¹^ORCID,Geyer Gerd²^ORCID,Bahrami Nasrin¹

Affiliation:

1. Department of Earth Sciences Institute for Advanced Studies in Basic Sciences (IASBS) Zanjan Iran

2. Lehrstuhl für Geodynamik und Geomaterialforsching, Institut für Geographie und Geologie Bayerische Julius‐Maximilians‐Universität Würzburg Germany

Publisher

Wiley

Subject

Geology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/gj.4624

Reference132 articles.

1. Cambrian Series 3 lithistid sponge-microbial reefs in Shandong Province, North China: reef development after the disappearance of archaeocyaths

2. Tectonostratigraphic synthesis and structural style of the alborz mountain system in Northern Iran

3. Stratigraphic and volcanic signatures of Miaolingian-Late Ordovician rift pulses in the Alborz Mountains, northern Iran

4. Batyrbay Section, South Kazakhstan, U.S.S.R. – potential stratotype for the Cambrian–Ordovician Boundary

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