Peridotites from the Izu-Bonin-Mariana Forearc (ODP Leg 125): Evidence for Mantle Melting and Melt-Mantle Interaction in a Supra-Subduction Zone Setting
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ID: 303785
1998
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Abstract
quartz) -1•1 (log units) and FMQ + 0•4 which ODP Leg 125; Izu-Bonin-Mariana forearc overlap those of mid-ocean ridge basalt (MORB) peridotites.Dunites from Conical Seamount contain small amounts of clinopyroxene, orthopyroxene and amphibole and are light REE (LREE) enriched.Moreover, they are considerably more oxidized than the harzburgites
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| Reference Key |
openalex_W2135015385
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|---|---|
| Authors | I. J. Parkinson, John A. Pearce |
| Journal | journal of petrology |
| Year | 1998 |
| DOI |
10.1093/petroj/39.9.1577
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| URL | |
| Keywords | Keywords not found |
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