Paleo-mantle wedge preserved in the Sambagawa high-pressure: Metamorphic belt and the thickness of forearc continental crust

Geology

Volumn 41, Issue 4, 2013, Pages 451-454

  Aoya, Mutsuki ^a   Endo, Shunsuke ^a   Mizukami, Tomoyuki ^b   Wallis, Simon R ^c  

^a NATIONAL INSTITUTE OF ADVANCED INDUSTRIAL SCIENCE AND TECHNOLOGY AIST   (Japan)

^b School of Natural System   (Japan)

^c NAGOYA UNIVERSITY   (Japan)

Author keywords

[No Author keywords available]

Indexed keywords

CONTINENTAL CRUSTS; EARTH'S SURFACE; MANTLE ROCKS; METAMORPHIC BELTS; METAMORPHIC PRESSURE; SAMBAGAWA BELT; SERPENTINITE; SUBDUCTION ZONES;

ROCKS;

METAMORPHIC ROCKS;

CONTINENTAL CRUST; CRUSTAL THICKNESS; FOREARC BASIN; GARNET; HIGH PRESSURE; MANTLE STRUCTURE; METAMORPHISM; METASEDIMENT; PERIDOTITE; SERPENTINITE; SUBDUCTION ZONE; TERRANE; ULTRAMAFIC ROCK;

JAPAN; SAMBAGAWA BELT;

EID: 84875511920     PISSN: 00917613     EISSN: 19432682     Source Type: Journal    
DOI: 10.1130/G33834.1     Document Type: Article

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