The δ 13 C – δ 18 O variations in marble in the Hida Belt, Japan-Reference-Cited by-同舟云学术

The δ 13 C – δ 18 O variations in marble in the Hida Belt, Japan

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

Author:

Harada Hironobu¹^ORCID,Tsujimori Tatsuki¹²^ORCID,Kunugiza Keitaro³^ORCID,Yamashita Katsuyuki⁴^ORCID,Aoki Shogo⁵⁶^ORCID,Aoki Kazumasa⁵^ORCID,Takayanagi Hideko¹^ORCID,Iryu Yasufumi¹^ORCID

Affiliation:

1. Graduate School of Science Tohoku University Sendai Japan

2. Center for Northeast Asian Studies Tohoku University Sendai Japan

3. Faculty of Human Development University of Toyama Toyama Japan

4. Graduate School of Natural Science and Technology Okayama University Okayama Japan

5. Center for Fundamental Education Okayama University of Science Okayama Japan

6. Graduate School of International Resource Sciences Akita University Akita Japan

Funder

Japan Society for the Promotion of Science

Publisher

Wiley

Subject

Geology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1111/iar.12389

Reference135 articles.

1. Constraint on the eclogite age of the Sanbagawa metamorphic rocks in central Shikoku, Japan

2. Oceanic-arc subduction, stagnation, and exhumation: zircon U–Pb geochronology and trace-element geochemistry of the Sanbagawa eclogites in central Shikoku, SW Japan

3. Rb-Sr ages of the gneiss and metamorphosed intrusive rocks of the Hida metamorphic belt in the Urushiyama area, Gifu Prefecture, central Japan.

4. Two types of granitic intrusions in the Hida belt, Japan: Sr isotopic and chemical characteristics of the Mesozoic Funatsu granitic rocks

5. Strontium isotopic compositions of Mesozoic granitic rocks in the Hida belt, central Japan: diversities of magma sources and of processes of magma evolution in a continental margin area

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