Cambrian supra-subduction and intraplate oceanic complexes in the Dzhalair-Naiman ophiolite zone (Southern Kazakhstan): age, geochemistry and tectonic implication-Reference-Cited by-同舟云学术

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Cambrian supra-subduction and intraplate oceanic complexes in the Dzhalair-Naiman ophiolite zone (Southern Kazakhstan): age, geochemistry and tectonic implication

Published:2024-10 Issue: Volume:134 Page:144-186
ISSN:1342-937X
Container-title:Gondwana Research
language:en
Short-container-title:Gondwana Research

Author:

Degtyarev Kirill E.,Tretyakov Andrey A.,Luchitskaya Marina V.,Ryazantsev Alexey V.^ORCID,Kanygina Nadezhda A.,Skoblenko Anfisa V.^ORCID,Tolmacheva Tatiana Yu,Yakubchuk Alexander S.,Milyukova Aleksandra G.^ORCID

Funder

Russian Academy of Sciences

Russian Science Foundation

Publisher

Elsevier BV

Reference149 articles.

1. Abdulin, A.A. (ed.), 1980. Chu-Ili Ore Belt: Geology of the Chu-Ili region. Alma-Ata: Nauka, 504 p. (in Russian).

2. The role of the Kazakhstan orocline in the late Paleozoic amalgamation of Eurasia;Abrajevich;Tectonophysics,2008

3. Geochemical data and zircon ages for rocks in a high-pressure belt of Chu-Yili Mountains, southern Kazakhstan: Implications for the earliest stages of accretion in Kazakhstan and the Tianshan;Alexeiev;J. Asian Earth Sci.,2011

4. Evolution of Cambrian and Early Ordovician arcs in the Kyrgyz North Tianshan: Insights from U-Pb zircon ages and geochemical data;Alexeiev;Gondwana Res.,2019

5. Tectonic setting for the genesis of oceanic plagiogranites: evidence from a paleo-spreading structure in the Oman ophiolite;Amri;Earth Planet. Sci. Lett,1996

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