Middle to Late Triassic granitic magmatism in the East Kunlun Orogenic Belt, NW China: Petrogenesis and implications for a transition from subduction to post‐collision setting of the Palaeo‐Tethys Ocean-Reference-Cited by-同舟云学术

Middle to Late Triassic granitic magmatism in the East Kunlun Orogenic Belt, NW China: Petrogenesis and implications for a transition from subduction to post‐collision setting of the Palaeo‐Tethys Ocean

Published:2021-02-24 Issue:6 Volume:56 Page:3378-3395
ISSN:0072-1050
Container-title:Geological Journal
language:en
Short-container-title:Geological Journal

Author:

Gao Hongchang¹^ORCID,Sun Fengyue¹

Affiliation:

1. College of Earth Sciences Jilin University Changchun China

Funder

National Natural Science Foundation of China

Publisher

Wiley

Subject

Geology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/gj.4104

Reference81 articles.

1. Correction of common lead in U–Pb analyses that do not report 204Pb

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

3. A review of the relationships between granitoid types, their origins and their geodynamic environments

4. Mineral/leucosome trace-element partitioning in a peraluminous migmatite (a laser ablation-ICP-MS study)

5. Age, geochemistry and tectonic setting of Buqingshan ophiolites, North Qinghai-Tibet Plateau, China

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