Duplex of metamorphic units including ultramafic rocks in the central region of Tokunoshima, Southwest Japan
Author:
Affiliation:
1. Graduate School of Science and Engineering; Kagoshima University; Kagoshima 890-0065 Japan
2. Faculty of Engineering; Kagawa University; Takamatsu 761-0396 Japan
Funder
Japan Society for the Promotion of Science
Publisher
Wiley
Subject
Geology
Link
http://onlinelibrary.wiley.com/wol1/doi/10.1111/iar.12199/fullpdf
Reference44 articles.
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3. Metamorphic belts of Japan;Banno;Episodes,1991
4. Orthogneiss, mylonite and non-coaxial deformation of granites: The example of the South Armorican shear zone;Berthé;Journal of Structural Geology,1979
5. Tectonic blocks in serpentinite mélange (eastern Cuba) reveal large-scale convective flow of the subduction channel;Blanco-Quintero;Geology,2011
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1. Dark cataclastic veins at the mouth of the Akirigami river in Tokunoshima, Southwest Japan;The Journal of the Geological Society of Japan;2023-12-22
2. Paleoproterozoic to Cenozoic zircon U–Pb ages with Hf signatures from metamorphic rocks and granodiorite of Tokunoshima: constraints on the geotectonic subdivision of the Ryukyu island arc, Southwest Japan;International Geology Review;2020-12-27
3. Growth and provenance of a Paleozoic subduction complex in the Broken River Province, Mossman Orogen: evidence from detrital zircon ages;Australian Journal of Earth Sciences;2019-02-22
4. Thematic section: Orogenic processes in island arcs: Subduction, accretion, collision and recycling;Island Arc;2018-12-26
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