Origin of high‐ Mg arc volcanism and fate of subducted sedimentary carbonates in the western Pacific: Evidence from partial melting experiments on mixed sediment and peridotite-Reference-Cited by-同舟云学术

Origin of high‐ Mg arc volcanism and fate of subducted sedimentary carbonates in the western Pacific: Evidence from partial melting experiments on mixed sediment and peridotite

Published:2021-10-28 Issue:1 Volume:57 Page:425-439
ISSN:0072-1050
Container-title:Geological Journal
language:en
Short-container-title:Geological Journal

Author:

Zhan Mingjun¹²,Zhang Guoliang¹³⁴

Affiliation:

1. Center of Deep Sea Research, Institute of Oceanology Chinese Academy of Sciences Qingdao China

2. University of Chinese Academy of Sciences Beijing China

3. Laboratory for Marine Geology Qingdao National Laboratory for Marine Science and Technology Qingdao China

4. Center for Ocean Mega‐Science Chinese Academy of Sciences Qingdao China

Funder

National Natural Science Foundation of China

Publisher

Wiley

Subject

Geology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/gj.4306

Reference85 articles.

1. Island arc magmatism in relation to the evolution of the crust and mantle

2. Partial melting in Archean subduction zones: constraints from experimentally determined trace element partition coefficients between eclogitic minerals and tonalitic melts under upper mantle conditions

3. Rare-earth element mobility during hydrothermal and metamorphic fluid-rock interaction and the significance of the oxidation state of europium

4. Garnet: Common Mineral, Uncommonly Useful

5. Tectonic and metasomatic mixing in a high-T, subduction-zone mélange—insights into the geochemical evolution of the slab–mantle interface

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1. Petrogenesis of late Cenozoic high Mg andesites with high Nb/Ta ratios in Northern Songliao Basin, NE China;Lithos;2023-01

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