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International Geology Review Volume 64, 2022 - Issue 2

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Research Article

The Siah Cheshmeh-Khoy-Misho-Tabriz fault (NW Iran) is a cryptic neotethys suture: evidence from detrital zircon geochronology, Hf isotopes, and provenance analysis

Ali Mohammadia Eurasia Institute of Earth Sciences, Istanbul Technical University, Maslak, Turkey;b Department of Earth Sciences, ETH Zurich, Zurich, SwitzerlandCorrespondence[email protected]
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Jean-Pierre Burgb Department of Earth Sciences, ETH Zurich, Zurich, SwitzerlandView further author information

Marcel Guillongb Department of Earth Sciences, ETH Zurich, Zurich, SwitzerlandView further author information

Pages 182-202 | Received 07 Jul 2020, Accepted 24 Oct 2020, Published online: 09 Dec 2020

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https://doi.org/10.1080/00206814.2020.1845992
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The Siah Cheshmeh-Khoy-Misho-Tabriz fault (NW Iran) is a cryptic neotethys suture: evidence from detrital zircon geochronology, Hf isotopes, and provenance analysis

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