Melting and Evolution of Amphibole‐Rich Back‐Arc Abyssal Peridotites at the Mado Megamullion, Shikoku Basin-Reference-Cited by-同舟云学术

Melting and Evolution of Amphibole‐Rich Back‐Arc Abyssal Peridotites at the Mado Megamullion, Shikoku Basin

Published:2021-12 Issue:12 Volume:22 Page:
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem Geophys Geosyst

Author:

Sen A.¹²^ORCID,Snow J. E.²,Ohara Y.³⁴⁵,Hirauchi K.⁶^ORCID,Kouketsu Y.⁵,Sanfilippo A.⁷^ORCID,Basch V.⁷^ORCID,Harigane Y.⁸^ORCID,Fujii M.⁹^ORCID,Okino K.¹⁰^ORCID,Akizawa N.¹⁰^ORCID

Affiliation:

1. Department of Earth and Atmospheric Sciences University of Houston Houston TX USA

2. Department of Geology and Geophysics Louisiana State University Baton Rouge LA USA

3. Hydrographic and Oceanographic Department of Japan Tokyo Japan

4. Research Institute for Marine Geodynamics Japan Agency for Marine‐Earth Science and Technology (JAMSTEC) Yokosuka Japan

5. Graduate School of Environmental Studies Nagoya University Nagoya Japan

6. Department of Geosciences Faculty of Science Shizuoka University Shizuoka Japan

7. Dipartimento di Scienze della Terra e dell'Ambiente University of Pavia Pavia Italy

8. Research Institute of Geology and Geoinformation Geological Survey of Japan National Institute of Advanced Industrial Science and Technology (AIST) Tsukuba Japan

9. National Institute of Polar Research/SOKENDAI Tokyo Japan

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

Funder

National Science Foundation

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2021GC010013

Reference124 articles.

1. Geochemical characteristics of back-arc basin lower crust and upper mantle at final spreading stage of Shikoku Basin: an example of Mado Megamullion