Ordovician supra-subduction, oceanic and within-plate ocean island complexes in the Tekturmas ophiolite zone (Central Kazakhstan): age, geochemistry and tectonic implications-Reference-Cited by-同舟云学术

Ordovician supra-subduction, oceanic and within-plate ocean island complexes in the Tekturmas ophiolite zone (Central Kazakhstan): age, geochemistry and tectonic implications

Published:2021-09-01 Issue: Volume: Page:1-43
ISSN:0020-6814
Container-title:International Geology Review
language:en
Short-container-title:International Geology Review

Author:

Degtyarev Kirill¹,Yakubchuk Alexander S.¹,Luchitskaya Marina V.¹,Tolmacheva Tatiana Yu.¹²,Skoblenko (Pilitsyna) Anfisa V.¹^ORCID,Tretyakov Andrey A.¹

Affiliation:

1. Department of Tectonics, Geological Institute, Russian Academy of Sciences, Moscow, Russia

2. Department of stratigraphy and paleontology, Karpinsky Russian Geological Research Institute (VSEGEI), St. Petersburg, Russia

Funder

Russian Science Foundation

Publisher

Informa UK Limited

Subject

Geology

Link

https://www.tandfonline.com/doi/pdf/10.1080/00206814.2021.1969691

Reference132 articles.

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3. Armstrong, H.A., Floyd, J.D., Barron, H.F., et al. 2001, Conodont biostratigraphy of the Crawford Group, Southern Uplands. British Geological Survey Research Report, 36 p.

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