Paleo-mantle wedge preserved in the Sambagawa high-pressure metamorphic belt and the thickness of forearc continental crust
Author:
Publisher
Geological Society of America
Subject
Geology
Link
http://pubs.geoscienceworld.org/geology/article-pdf/41/4/451/3545298/451.pdf
Reference23 articles.
1. Geology of the Hibihara district;Aoya,2009
2. High-P metamorphism, pattern of induced flow in the mantle wedge, and the link with plutonism in paired metamorphic belts;Aoya;Terra Nova,2009
3. Dynamics of petrogenesis;Banno,2000
4. Thin crust, ultramafic exposures, and rugged faulting patterns at the Mid-Atlantic Ridge (22°–24°N);Cannat;Geology,1995
5. Paragenesis of sodic pyroxene-bearing quartz schist: Implications for the P-T history of the Sanbagawa belt;Enami;Contributions to Mineralogy and Petrology,1994
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