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Radhakrishna, T., Divakara Rao, V., Krishna Rao, J. R. S. (1982) Occurrence and significance of awaruite in the Dras ultramafics, Kashmir Himalaya, India. Mineralogical Magazine, 46 (341) 483-484 doi:10.1180/minmag.1982.046.341.13

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Reference TypeJournal (article/letter/editorial)
TitleOccurrence and significance of awaruite in the Dras ultramafics, Kashmir Himalaya, India
JournalMineralogical MagazineISSN0026-461X
AuthorsRadhakrishna, T.Author
Divakara Rao, V.Author
Krishna Rao, J. R. S.Author
Year1982 (December)Volume46
Issue341
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_46/46-341-483.pdf+
DOIdoi:10.1180/minmag.1982.046.341.13Search in ResearchGate
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Mindat Ref. ID3442Long-form Identifiermindat:1:5:3442:9
GUID0
Full ReferenceRadhakrishna, T., Divakara Rao, V., Krishna Rao, J. R. S. (1982) Occurrence and significance of awaruite in the Dras ultramafics, Kashmir Himalaya, India. Mineralogical Magazine, 46 (341) 483-484 doi:10.1180/minmag.1982.046.341.13
Plain TextRadhakrishna, T., Divakara Rao, V., Krishna Rao, J. R. S. (1982) Occurrence and significance of awaruite in the Dras ultramafics, Kashmir Himalaya, India. Mineralogical Magazine, 46 (341) 483-484 doi:10.1180/minmag.1982.046.341.13
In(1982, December) Mineralogical Magazine Vol. 46 (341) Mineralogical Society
Abstract/NotesAbstractA new occurrence of awaruite, from India, is reported in the ultramafic units of the Dras area which form part of the Indus Suture ophiolites in Kashmir Himalaya. Its formation in these rocks suggests a low-temperature process of serpentinization. Ni and Fe released from olivine and/or pyroxene must have formed awaruite peragenetically next to magnetite and pentlandite.

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LocalityCitation Details
Dras ultramafics, Kargil district, Ladakh, India

Mineral Occurrences

LocalityMineral(s)
Dras ultramafics, Kargil district, Ladakh, India Awaruite, Chromite, Magnetite, Pentlandite, Serpentine Subgroup


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