Orthopyroxenes from Sukinda ultramafites and the nature of the parental magma
Chromite-bearing ultramafites occur as synkinematic intrusions during the Eastern Ghat orogenic movement (2800—3000 m. y.), in Eastern India. The ultramafic instrusives are composed mainly of dunite, bronzitites, websterite and their metamorphic derivatives. These were emplaced by successive 'p...
Elmentve itt :
Szerző: | Mitra Sachinath |
---|---|
Dokumentumtípus: | Cikk |
Megjelent: |
University of Szeged, Department of Mineralogy, Geochemistry and Petrology
Szeged
1973
|
Sorozat: | Acta mineralogica-petrographica
21 No. 1 |
Kulcsszavak: | Kőzettan, Ásványtan, Földtan |
Tárgyszavak: | |
Online Access: | http://acta.bibl.u-szeged.hu/24562 |
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