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Kocks, H., Melcher, F., Meisel, T., Burgath, K.-P. (2007) Diverse contributing sources to chromitite petrogenesis in the Shebenik Ophiolitic Complex, Albania: evidence from new PGE- and Os-isotope data. Mineralogy and Petrology, 91 (3) 139-170 doi:10.1007/s00710-007-0194-4

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Reference TypeJournal (article/letter/editorial)
TitleDiverse contributing sources to chromitite petrogenesis in the Shebenik Ophiolitic Complex, Albania: evidence from new PGE- and Os-isotope data
JournalMineralogy and Petrology
AuthorsKocks, H.Author
Melcher, F.Author
Meisel, T.Author
Burgath, K.-P.Author
Year2007 (November)Volume91
Issue3
PublisherSpringer Science and Business Media LLC
DOIdoi:10.1007/s00710-007-0194-4Search in ResearchGate
Generate Citation Formats
Mindat Ref. ID16816Long-form Identifiermindat:1:5:16816:8
GUID0
Full ReferenceKocks, H., Melcher, F., Meisel, T., Burgath, K.-P. (2007) Diverse contributing sources to chromitite petrogenesis in the Shebenik Ophiolitic Complex, Albania: evidence from new PGE- and Os-isotope data. Mineralogy and Petrology, 91 (3) 139-170 doi:10.1007/s00710-007-0194-4
Plain TextKocks, H., Melcher, F., Meisel, T., Burgath, K.-P. (2007) Diverse contributing sources to chromitite petrogenesis in the Shebenik Ophiolitic Complex, Albania: evidence from new PGE- and Os-isotope data. Mineralogy and Petrology, 91 (3) 139-170 doi:10.1007/s00710-007-0194-4
In(2007, November) Mineralogy and Petrology Vol. 91 (3) Springer Science and Business Media LLC

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Uysal, I., Sadiklar, M. B., Tarkian, M., Karsli, O., Aydin, F. (2005) Mineralogy and composition of the chromitites and their platinum-group minerals from Ortaca (Mu?la-SW Turkey): evidence for ophiolitic chromitite genesis. Mineralogy and Petrology, 83 (3) 219-242 doi:10.1007/s00710-004-0063-3
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Uysal, I., Sadiklar, M. B., Tarkian, M., Karsli, O., & Aydin, F. (2005). Mineralogy and composition of the chromitites and their platinum-group minerals from Ortaca (MuÄŸla-SW Turkey): evidence for ophiolitic chromitite genesis. Mineralogy and petrology, 83(3-4), 219-242.
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