Makran ophiolitic basalts (SE Iran) record Late Cretaceous Neotethys plume-ridge interaction-Reference-Cited by-同舟云学术

Makran ophiolitic basalts (SE Iran) record Late Cretaceous Neotethys plume-ridge interaction

Published:2019-09-02 Issue:13-14 Volume:62 Page:1677-1697
ISSN:0020-6814
Container-title:International Geology Review
language:en
Short-container-title:International Geology Review

Author:

Esmaeili Rasoul¹²,Xiao Wenjiao¹²³⁴^ORCID,Ebrahimi Mohammad⁵,Zhang Ji’En¹,Zhang Zhiyong¹,Abd El-Rahman Yasser⁶,Han Chunming¹⁴,Wan Bo¹⁴,Ao Songjian¹,Song Dongfang¹,Shahabi Shirin⁷,Aouizerat Arthur¹²

Affiliation:

1. State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, China

2. University of Chinese Academy of Sciences, Beijing, China

3. Xinjiang Research Center for Mineral Resources, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi, China

4. CAS Center for Excellence in Tibetan Plateau Earth Science, Chinese Academy of Sciences, Beijing, China

5. Department of Geology, Faculty of Sciences, University of Zanjan, Zanjn, Iran

6. Geology Department, Faculty of Science, Cairo University, Giza, Egypt

7. Geology Department, Faculty of Science, Shahrood University of technology, Shahrood, Iran

Funder

The Key Research Program of Frontier Sciences, CAS

The National Natural Science Foundation of china

The Strategic Priority Research Program (B) of the Chinese Academy of Sciences

Publisher

Informa UK Limited

Subject

Geology

Link

https://www.tandfonline.com/doi/pdf/10.1080/00206814.2019.1658232

Reference105 articles.

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

2. U–Pb zircon ages, field geology and geochemistry of the Kermanshah ophiolite (Iran): From continental rifting at 79Ma to oceanic core complex at ca. 36Ma in the southern Neo-Tethys

3. Geochemistry of arc volcanic rocks of the Zagros Crush Zone, Neyriz, Iran

4. Petrogenesis of Quaternary Intraplate Volcanism, Sana'a, Yemen: Implications for Plume-Lithosphere Interaction and Polybaric Melt Hybridization

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