Sediment-infill volcanic breccia from the Neoarchean Shimoga greenstone terrane, western Dharwar Craton: implications on pyroclastic volcanism and sedimentation in an active continental margin

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dc.contributor.authorManikyamba, C.
dc.contributor.authorSaha, A.
dc.contributor.authorGanguly, S.
dc.contributor.authorSantosh, M.
dc.contributor.authorLingadevaru, M.
dc.contributor.authorRajanikanta Singh, M.
dc.contributor.authorSubba Rao, D.
dc.date.issued2014
dc.description.abstractAbstract not available
dc.description.statementofresponsibilityC. Manikyamba, Abhishek Saha, Sohini Ganguly, M. Santosh, M. Lingadevaru, M. Rajanikanta Singh, D.V. Subba Rao
dc.identifier.citationJournal of Asian Earth Sciences, 2014; 96:269-278
dc.identifier.doi10.1016/j.jseaes.2014.09.008
dc.identifier.issn1367-9120
dc.identifier.issn1878-5786
dc.identifier.orcidSantosh, M. [0000-0002-1073-8477]
dc.identifier.urihttp://hdl.handle.net/2440/105026
dc.language.isoen
dc.publisherElsevier
dc.relation.grantMLP 6201-28
dc.rights© 2014 Elsevier Ltd. All rights reserved.
dc.source.urihttps://doi.org/10.1016/j.jseaes.2014.09.008
dc.subjectSediment-infill volcanic breccia; pyroclastic rocks; active continental margin; Shimoga greenstone belt; Dharwar Craton
dc.titleSediment-infill volcanic breccia from the Neoarchean Shimoga greenstone terrane, western Dharwar Craton: implications on pyroclastic volcanism and sedimentation in an active continental margin
dc.typeJournal article
pubs.publication-statusPublished

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