High-Mg low-Ni olivine cumulates from a Pan-African accretionary belt in southern India: Implications for the genesis of volatile-rich high-Mg melts in suprasubduction setting

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dc.contributor.authorRajesh, V.
dc.contributor.authorArai, S.
dc.contributor.authorSatish-kumar, M.
dc.contributor.authorSantosh, M.
dc.contributor.authorTamura, A.
dc.date.issued2013
dc.description.abstractAbstract not available
dc.description.statementofresponsibilityV.J. Rajesh, S. Arai, M. Satish-kumar, M. Santosh, A. Tamura
dc.identifier.citationPrecambrian Research, 2013; 227:409-425
dc.identifier.doi10.1016/j.precamres.2012.08.004
dc.identifier.issn0301-9268
dc.identifier.issn1872-7433
dc.identifier.orcidSantosh, M. [0000-0002-1073-8477]
dc.identifier.urihttp://hdl.handle.net/2440/99062
dc.language.isoen
dc.publisherElsevier B.V.
dc.rights© 2012 Elsevier B.V. All rights reserved.
dc.source.urihttps://doi.org/10.1016/j.precamres.2012.08.004
dc.subjectSpinel dunite; Petrology; Geochemistry; Stable isotopes; Subduction; Accretion; Southern India
dc.titleHigh-Mg low-Ni olivine cumulates from a Pan-African accretionary belt in southern India: Implications for the genesis of volatile-rich high-Mg melts in suprasubduction setting
dc.typeJournal article
pubs.publication-statusPublished

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