Early Eocene A-type (ferroan) rhyolites in southwestern Tibet: A far-field tectonic effect of the India–Eurasia collision
Author:
Affiliation:
1. College of Earth Sciences, Chengdu University of Technology, Chengdu, 610059, China
2. School of Earth Sciences, Yunnan University, Kunming, 650500, China
3. Geosciences Department, University of Texas at Dallas, Richardson, TX 75080, USA
Funder
Chengdu University of Technology
National Natural Science Foundation of China
Sichuan Science and Technology Program
Yunnan University
Publisher
Informa UK Limited
Subject
Geology
Link
https://www.tandfonline.com/doi/pdf/10.1080/00206814.2022.2117740
Reference135 articles.
1. Far-field tectonic effects of the Arabia–Eurasia collision and the inception of the North Anatolian Fault system
2. Eocene Granitic Magmatism in NW Anatolia (Turkey) revisited: New implications from comparative zircon SHRIMP U–Pb and 40Ar–39Ar geochronology and isotope geochemistry on magma genesis and emplacement
3. Controls on the fractionation of isovalent trace elements in magmatic and aqueous systems: evidence from Y/Ho, Zr/Hf, and lanthanide tetrad effect
4. Deformation and cooling history of the Central Qiangtang terrane, Tibetan Plateau and its tectonic implications
5. Cratons, mobile belts, alkaline rocks and continental lithospheric mantle: the Pan-African testimony
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