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...

Teljes leírás

Elmentve itt :
Bibliográfiai részletek
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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