Crustal anorthosite formation by deep‐seated hydrothermal circulation beneath fast‐spreading axis: Constraints from chronological approach, Sr isotope, and fluid–chromite inclusion investigation-Reference-Cited by-同舟云学术

Crustal anorthosite formation by deep‐seated hydrothermal circulation beneath fast‐spreading axis: Constraints from chronological approach, Sr isotope, and fluid–chromite inclusion investigation

Published:2021-01 Issue:1 Volume:30 Page:
ISSN:1038-4871
Container-title:Island Arc
language:en
Short-container-title:Island Arc

Author:

Akizawa Norikatsu¹^ORCID,Miyake Akira²^ORCID,Igami Yohei²^ORCID,Tsuchiyama Akira³⁴⁵^ORCID,Asanuma Hisashi¹⁶^ORCID,Kogiso Tetsu⁷^ORCID,Wakaki Shigeyuki⁸^ORCID,Ishikawa Tsuyoshi⁸^ORCID,Arai Shoji⁹^ORCID,Eom Jiwon¹^ORCID,Kawahata Hodaka¹^ORCID,Aze Takahiro¹^ORCID,Yokoyama Yusuke¹^ORCID

Affiliation:

1. Atmosphere and Ocean Research Institute The University of Tokyo Chiba Japan

2. Graduate School of Science Kyoto University Kyoto Japan

3. Research Organization of Science and Technology Ritsumeikan University Kusatsu Japan

4. Guangzhou Institute of Geochemistry Chinese Academy of Sciences Guangzhou China

5. Center for Excellence in Deep Earth Science Chinese Academy of Sciences Guangzhou China

6. Geochemical Research Center The University of Tokyo Tokyo Japan

7. Graduate School of Human and Environmental Studies Kyoto University Kyoto Japan

8. Kochi Institute for Core Sample Research Japan Agency for Marine‐Earth Science and Technology (JAMSTEC) Nankoku Japan

9. Department of Earth Sciences Kanazawa University Kanazawa Japan

Funder

Kurita Water and Environment Foundation

Ministry of Education, Culture, Sports, Science and Technology

Publisher

Wiley

Subject

Geology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1111/iar.12423

Reference125 articles.

1. Geology and petrology of the plutonic complexes in the Wadi Fizh area: Multiple magmatic events and segment structure in the northern Oman ophiolite

2. Petrologic profile of peridotite layers under a possible Moho in the northern Oman ophiolite: an example from Wadi Fizh

3. Petrology of mantle diopsidite from Wadi Fizh, northern Oman ophiolite: Cr and REE mobility by hydrothermal solution

4. Behavior of MORB magmas at uppermost mantle beneath a fast-spreading axis: an example from Wadi Fizh of the northern Oman ophiolite

5. Crustal diopsidites from the northern Oman ophiolite: Evidence for hydrothermal circulation through suboceanic Moho

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