Late Eocene slab retreat, extension, and mantle upwelling inferred from mantle signatures in potassium-rich magmatism in NE Iran-Reference-Cited by-同舟云学术

Late Eocene slab retreat, extension, and mantle upwelling inferred from mantle signatures in potassium-rich magmatism in NE Iran

Published:2023-03-06 Issue:9 Volume:65 Page:1586-1600
ISSN:0020-6814
Container-title:International Geology Review
language:en
Short-container-title:International Geology Review

Author:

Alizadeh Elahe¹²,Li Huan³^ORCID,Babazadeh Shahrouz⁴,Ma Changqian⁵⁶,Förster Michael W.⁷

Affiliation:

1. Department of Geology, Faculty of Sciences, University of Hormozgan, Bandar Abbas, Iran

2. Iran Minerals Production and Supply Company (IMPASCO), Tehran, Iran

3. Key Laboratory of Metallogenic Prediction of Nonferrous Metals and Geological Environment Monitoring, Ministry of Education, School of Geosciences and Info-Physics, Central South University, Changsha, China

4. Research Institute for Earth Sciences, Geological Survey of Iran, Tehran, Iran

5. Faculty of Earth Sciences, China University of Geosciences, Wuhan, China

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

7. School of Natural Sciences, Macquarie University, Sydney, Australia

Funder

evaluation model of resources potential for copper, nickel, and uranium in Western Asia

Publisher

Informa UK Limited

Subject

Geology

Link

https://www.tandfonline.com/doi/pdf/10.1080/00206814.2023.2185823

Reference80 articles.

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4. Origin of 1.8 Ga zircons in Post Eocene mafic dikes in the Roshtkhar area, NE Iran

5. Geochemical and Sr–Nd–Pb isotopic characteristics of Paleocene plagioleucitites from the Eastern Pontides (NE Turkey)

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