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Tectonic Implications of the Composition of Volcanic ARC Magmas

✍ Scribed by Pearce, J. A.; Peate, D. W.


Book ID
111679728
Publisher
Annual Reviews
Year
1995
Tongue
English
Weight
995 KB
Volume
23
Category
Article
ISSN
0084-6597

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✦ Synopsis


that the mantle wedge experiences subduction-induced corner flow (e.g. Spiegelman & MacKenzie 1987); 2. that the subduction component reaches the fusible part of the mantle wedge by the three-stage process of (i) metasomatism of mantle lithosphere, fol lowed by (ii) aqueous fluid release due to breakdown of hydrous minerals at depth (e.g. Wyllie 1983, Tatsumi et al 1983) and (iii) aqueous fluid migra tion, followed by hydrous melt migration, to the site of melting;


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