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Marchesi, Claudio, González-Jiménez, José María, Gervilla, Fernando, Garrido, Carlos J., Griffin, William L., O’Reilly, Suzanne Y., Proenza, Joaquín A., Pearson, Norman J. (2011) In situ Re–Os isotopic analysis of platinum-group minerals from the Mayarí-Cristal ophiolitic massif (Mayarí-Baracoa Ophiolitic Belt, eastern Cuba): implications for the origin of Os-isotope heterogeneities in podiform chromitites. Contributions to Mineralogy and Petrology, 161 (6) 977-990 doi:10.1007/s00410-010-0575-2

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Reference TypeJournal (article/letter/editorial)
TitleIn situ Re–Os isotopic analysis of platinum-group minerals from the Mayarí-Cristal ophiolitic massif (Mayarí-Baracoa Ophiolitic Belt, eastern Cuba): implications for the origin of Os-isotope heterogeneities in podiform chromitites
JournalContributions to Mineralogy and Petrology
AuthorsMarchesi, ClaudioAuthor
González-Jiménez, José MaríaAuthor
Gervilla, FernandoAuthor
Garrido, Carlos J.Author
Griffin, William L.Author
O’Reilly, Suzanne Y.Author
Proenza, Joaquín A.Author
Pearson, Norman J.Author
Year2011 (June)Volume161
Issue6
PublisherSpringer Science and Business Media LLC
DOIdoi:10.1007/s00410-010-0575-2Search in ResearchGate
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Mindat Ref. ID79176Long-form Identifiermindat:1:5:79176:2
GUID0
Full ReferenceMarchesi, Claudio, González-Jiménez, José María, Gervilla, Fernando, Garrido, Carlos J., Griffin, William L., O’Reilly, Suzanne Y., Proenza, Joaquín A., Pearson, Norman J. (2011) In situ Re–Os isotopic analysis of platinum-group minerals from the Mayarí-Cristal ophiolitic massif (Mayarí-Baracoa Ophiolitic Belt, eastern Cuba): implications for the origin of Os-isotope heterogeneities in podiform chromitites. Contributions to Mineralogy and Petrology, 161 (6) 977-990 doi:10.1007/s00410-010-0575-2
Plain TextMarchesi, Claudio, González-Jiménez, José María, Gervilla, Fernando, Garrido, Carlos J., Griffin, William L., O’Reilly, Suzanne Y., Proenza, Joaquín A., Pearson, Norman J. (2011) In situ Re–Os isotopic analysis of platinum-group minerals from the Mayarí-Cristal ophiolitic massif (Mayarí-Baracoa Ophiolitic Belt, eastern Cuba): implications for the origin of Os-isotope heterogeneities in podiform chromitites. Contributions to Mineralogy and Petrology, 161 (6) 977-990 doi:10.1007/s00410-010-0575-2
In(2011, June) Contributions to Mineralogy and Petrology Vol. 161 (6) Springer Science and Business Media LLC


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