Formation of secondary olivine after orthopyroxene during hydration of mantle wedge: evidence from the Khantaishir Ophiolite, western Mongolia
Author:
Funder
Japan Society for the Promotion of Science
Publisher
Springer Science and Business Media LLC
Subject
Geochemistry and Petrology,Geophysics
Link
http://link.springer.com/content/pdf/10.1007/s00410-019-1623-1.pdf
Reference83 articles.
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2. Arcay D, Tric E, Doin M-P (2005) Numerical simulations of subduction zones: effect of slab dehydration on the mantle wedge dynamics. Phys Earth Planet Inter 149:133–153
3. Badarch G, Dickson-Cunningham W, Windley BF (2002) A new terrane subdivision for Mongolia: implications for the Phanerozoic crustal growth of Central Asia. J Asian Earth Sci 21:87–110
4. Bostock MG, Hyndman RD, Rondenay S, Peacock SM (2002) An inverted continental Moho and serpentinization of the forearc mantle. Nature 417:536–538
5. Bowin CO, Nalwalk AJ, Hersey JB (1996) Serpentinized peridotite from the north wall of the Puerto Rico trench. Geol Soc Am Bull 77:257–270
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