Suprasubduction zone ophiolite from Agali hill: Petrology, zircon SHRIMP U-Pb geochronology, geochemistry and implications for Neoarchean plate tectonics in southern India

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dc.contributor.authorSantosh, M.
dc.contributor.authorShaji, E.
dc.contributor.authorTsunogae, T.
dc.contributor.authorRam Mohan, M.
dc.contributor.authorSatyanarayanan, M.
dc.contributor.authorHorie, K.
dc.date.issued2013
dc.description.abstractAbstract not available
dc.description.statementofresponsibilityM. Santosha, E. Shajib, T. Tsunogaec, M. Ram Mohand, M. Satyanarayanand, K. Horiee
dc.identifier.citationPrecambrian Research, 2013; 231:301-324
dc.identifier.doi10.1016/j.precamres.2013.04.003
dc.identifier.issn0301-9268
dc.identifier.issn1872-7433
dc.identifier.orcidSantosh, M. [0000-0002-1073-8477]
dc.identifier.urihttp://hdl.handle.net/2440/104576
dc.language.isoen
dc.publisherElsevier
dc.rights© 2013 Elsevier B.V. All rights reserved.
dc.source.urihttps://doi.org/10.1016/j.precamres.2013.04.003
dc.subjectSuprasubduction zone ophiolite; geochemistry; geochronology; Neoarchean continental growth; southern India
dc.titleSuprasubduction zone ophiolite from Agali hill: Petrology, zircon SHRIMP U-Pb geochronology, geochemistry and implications for Neoarchean plate tectonics in southern India
dc.typeJournal article
pubs.publication-statusPublished

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