A petrologic and isotopic study of lodranites: Evidence for early formation as partial melt residues from heterogeneous precursors

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dc.contributor.authorMcCoy, Timothy J.
dc.contributor.authorKeil, K.
dc.contributor.authorClayton, R. N.
dc.contributor.authorMayeda, T. K.
dc.contributor.authorBogard, D. D.
dc.contributor.authorGarrison, D. H.
dc.contributor.authorWieler, R.
dc.date.accessioned2013-04-22T18:25:38Z
dc.date.available2013-04-22T18:25:38Z
dc.date.issued1997
dc.format.extent623–637
dc.identifier.citationMcCoy, Timothy J., Keil, K., Clayton, R. N., Mayeda, T. K., Bogard, D. D., Garrison, D. H., and Wieler, R. 1997. "<a href="https://repository.si.edu/handle/10088/20526">A petrologic and isotopic study of lodranites: Evidence for early formation as partial melt residues from heterogeneous precursors</a>." <em>Geochim.Cosmochim.Acta</em>, 61 623–637.
dc.identifier.urihttp://hdl.handle.net/10088/20526
dc.relation.ispartofGeochim.Cosmochim.Acta 61
dc.titleA petrologic and isotopic study of lodranites: Evidence for early formation as partial melt residues from heterogeneous precursors
dc.typearticle
sro.description.unitNMNH
sro.description.unitNH-Mineral Sciences
sro.description.unitAnnals-Import
sro.identifier.itemID96217
sro.identifier.refworksID58871
sro.identifier.urlhttps://repository.si.edu/handle/10088/20526

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