B-type olivine fabrics developed in the fore-arc side of the mantle wedge along a subducting slab

Earth and Planetary Science Letters

Volumn 272, Issue 3-4, 2008, Pages 747-757

  Tasaka, Miki ^a   Michibayashi, Katsuyoshi ^b   Mainprice, David ^c  

^a UNIVERSITY OF TOKYO   (Japan)

^b SHIZUOKA UNIVERSITY   (Japan)

^c UNIVERSITÉ MONTPELLIER 2   (France)

Author keywords

B type olivine fabric; dunite; hydration; mantle wedge; seismic anisotropy; subduction

Indexed keywords

ATOMIC RATIOS; BONINITE; CHROMIAN SPINEL; EVOLUTION (CO); MANTLE WEDGE; METAMORPHIC BELTS; SOUTHWEST (CO); SUBDUCTING SLABS;

DUNITE; FOREARC BASIN; HYDRATION; MICROSTRUCTURE; OLIVINE; P-WAVE; RETROGRESSION; S-WAVE; SEISMIC ANISOTROPY; SEISMIC PROPERTY; SLAB; SUBDUCTION ZONE; TECTONIC WEDGE;

ASIA; EURASIA; FAR EAST; JAPAN; SAMBAGAWA BELT;

EID: 48149115487     PISSN: 0012821X     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.epsl.2008.06.014     Document Type: Article

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