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Cited by 919

The DOI matches its Crossref record; 2 of the 2 references it cites were found in a registry or an index.

Peridotites from the Izu-Bonin-Mariana Forearc (ODP Leg 125): Evidence for Mantle Melting and Melt-Mantle Interaction in a Supra-Subduction Zone Setting

Parkinson, I. J., Pearce, J. A.·1998·Journal of Petrology

Abstract

KEY WORDS: mantle peridotites; mantle melting; supra-subduction zone; magnetite-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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Metadata

Authors
Parkinson, I. J., & Pearce, J. A.
Venue
Journal of Petrology
Published
1998-09-01
Volume
39
Issue
9
Pages
1577-1618
ISSN
  • 0022-3530 (ISSN-L)
  • 1460-2415
OpenAlex
W2135015385
Cited by
919
References
2
FWCI
10.41
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Peridotites from the Izu-Bonin-Mariana Forearc (ODP Leg 125): Evidence for Mantle Melting and Melt-Mantle Interaction in a Supra-Subduction Zone Setting. https://app.cochat.ai/papers/10.1093/petroj/39.9.1577
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Parkinson, I. J., & Pearce, J. A. (1998). Peridotites from the Izu-Bonin-Mariana Forearc (ODP Leg 125): Evidence for Mantle Melting and Melt-Mantle Interaction in a Supra-Subduction Zone Setting. Journal of Petrology. https://doi.org/10.1093/petroj/39.9.1577

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