Transition in tectonic regime from the Paleo-Asian Ocean to Paleo-Pacific Ocean: constraints from the Jurassic adakitic and I-type granites, and calc-alkaline diorites at the northern margin of the North China Craton-Reference-Cited by-同舟云学术

Transition in tectonic regime from the Paleo-Asian Ocean to Paleo-Pacific Ocean: constraints from the Jurassic adakitic and I-type granites, and calc-alkaline diorites at the northern margin of the North China Craton

Published:2021-02-15 Issue: Volume: Page:1-32
ISSN:0020-6814
Container-title:International Geology Review
language:en
Short-container-title:International Geology Review

Author:

Jing Yan¹²,Ge Wen-Chun¹²,Dong Yu¹²,Yang Hao¹²,Ji Zheng¹²^ORCID,Bi Jun-Hui³,Zhou Hong-Ying³,Xing De-He⁴

Affiliation:

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

2. Key Laboratory of Mineral Resources Evaluation in Northeast Asia, Ministry of Land and Resources of China, Changchun, China

3. China Geological Survey, Tianjin Center, Tianjin, China

4. China Geological Survey, Shenyang Center, Shenyang, China

Funder

National Natural Science Foundation of China

Graduate Innovation Fund of Jilin University

Publisher

Informa UK Limited

Subject

Geology

Link

https://www.tandfonline.com/doi/pdf/10.1080/00206814.2020.1867913

Reference149 articles.

1. Characteristics of Jurassic Continental Arc Magmatism in South Korea: Tectonic Implications

2. Late Paleozoic to Early Mesozoic arc-related magmatism in southeastern Korea: SHRIMP zircon geochronology and geochemistry

3. Early-middle archaean crustal evolution deduced from Lu-Hf and U-Pb isotopic studies of single zircon grains

4. Generation of sodium-rich magmas from newly underplated basaltic crust

5. Igneous zircon: trace element composition as an indicator of source rock type

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