Isotopic evidence for channeled fluid flow in low-grade metamorphosed Jurassic accretionary complex in the Northern Chichibu belt, western Shikoku, Japan-Reference-Cited by-同舟云学术

Isotopic evidence for channeled fluid flow in low-grade metamorphosed Jurassic accretionary complex in the Northern Chichibu belt, western Shikoku, Japan

Published:2007-03 Issue:3 Volume:25 Page:383-400
ISSN:0263-4929
Container-title:Journal of Metamorphic Geology
language:en
Short-container-title:J Metamorph Geol

Author:

SAKAKIBARA M.,UMEKI M.,CARTWRIGHT I.

Publisher

Wiley

Subject

Geochemistry and Petrology,Geology

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1111/j.1525-1314.2007.00701.x/fullpdf

Reference93 articles.

1. Sanbagawa metamorphism of the Nakatsu-Nanokawa district, the northern subbelt of the Chichibu belt in western central Shikoku

2. Pumpellyite–actinolite facies of the Sanbagawa metamorphism

3. Focused fluid flow during subduction: Oxygen isotope data from high-pressure ophiolites of the western Alps

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