Amalgamation of the Ryoke and Sanbagawa metamorphic belts at the subduction interface: New insights from the Kashio mylonite along the Median Tectonic Line, Nagano, Japan
Author:
Affiliation:
1. Geological Survey of Japan, AIST Tsukuba Japan
2. Kyoto Fission‐Track Co., Ltd. Kyoto Japan
3. Geochemical Research Center, Graduate School of Science The University of Tokyo Tokyo Japan
Funder
Japan Society for the Promotion of Science
Publisher
Wiley
Subject
Geochemistry and Petrology,Geology
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1111/jmg.12633
Reference113 articles.
1. The effects of temperature and fO2on the Al-in-hornblende barometer
2. Recognition of the Shimanto HP metamorphic belt within the traditional Sanbagawa HP metamorphic belt: New perspectives of the Cretaceous–Paleogene tectonics in Japan
3. P–T–D Path of Eclogite from the Sambagawa Belt Deduced from Combination of Petrological and Microstructural Analyses
4. Recognition of the ‘early’ Sambagawa metamorphism and a schematic cross-section of the Late-Cretaceous Sambagawa subduction zone
5. High-Pmetamorphism, pattern of induced flow in the mantle wedge, and the link with plutonism in paired metamorphic belts
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