Flow kinematics in the deeper part of a subduction channel, as inferred from inclusion trails in plagioclase porphyroblasts from the Sambagawa metamorphic rocks, south-west Japan
Author:
Publisher
Wiley
Subject
Geochemistry and Petrology,Geology
Link
http://onlinelibrary.wiley.com/wol1/doi/10.1111/j.1525-1314.2005.00576.x/fullpdf
Reference66 articles.
1. Intermediate high-pressure exhumation of the northern segment of the Sanbagawa belt, Saruta-gawa area, central Shikoku, Japan
2. THERMAL STRUCTURE OF THE SANBAGAWA METAMORPHIC BELT IN CENTRAL SHIKOKU
3. Pressure-temperature trajectory of the Sanbagawa metamorphism deduced from garnet zoning
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2. Exhumation of oceanic blueschists and eclogites in subduction zones: Timing and mechanisms;Earth-Science Reviews;2009-01
3. The high P/T Sambagawa extrusional wedge, Japan;Journal of Structural Geology;2007-07
4. Tectono-metamorphic history of the Tacagua ophiolitic unit (Cordillera de la Costa, northern Venezuela): Insights in the evolution of the southern margin of the Caribbean Plate;Island Arc;2007-03
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