Geochronological and geochemical constraints on the Erguna massif basement, NE China – subduction history of the Mongol–Okhotsk oceanic crust-Reference-Cited by-同舟云学术

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Geochronological and geochemical constraints on the Erguna massif basement, NE China – subduction history of the Mongol–Okhotsk oceanic crust

Published:2013-06-10 Issue:14 Volume:55 Page:1801-1816
ISSN:0020-6814
Container-title:International Geology Review
language:en
Short-container-title:International Geology Review

Author:

Sun De-You¹,Gou Jun¹,Wang Tian-Hao¹,Ren Yun-Sheng¹,Liu Yong-Jiang¹,Guo Hong-Yu¹,Liu Xiao-Ming²,Hu Zhao-Chu³

Affiliation:

1. College of Earth Sciences, Jilin University, Changchun 130061, China

2. State Key Laboratory of Continental Dynamics, Northwest University, Xi’an 710069, China

3. State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, China

Publisher

Informa UK Limited

Subject

Geology

Link

https://www.tandfonline.com/doi/pdf/10.1080/00206814.2013.804664

Reference63 articles.

1. Cosmochemistry of the Rare Earth Elements: Meteorite Studies

2. Evolution of the Solonker suture zone: Constraints from zircon U–Pb ages, Hf isotopic ratios and whole-rock Nd–Sr isotope compositions of subduction- and collision-related magmas and forearc sediments

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3. Late Mesozoic stratigraphic framework of the Great Xing’an Range, NE China, and overprinting by the Mongol–Okhotsk and Paleo-Pacific tectonic regimes;Gondwana Research;2024-10

4. Petrogenesis of the Early Jurassic–Early Cretaceous Adakite-like Rocks in the Erguna Block, NE China: Implications for the Tectonic Evolution of the Mongol–Okhotsk Ocean;Minerals;2024-07-19

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