Evidence of garnet to spinel peridotite transition In the harzburgites of Indus ophiolite belt: An indication of their mantle origin

dc.contributor.author	Karmalkar, N.R.
dc.contributor.author	Dessai, A.G.
dc.contributor.author	Duraiswami, R.A.
dc.contributor.author	Leblanc, M.
dc.date.accessioned	2015-06-03T06:47:03Z
dc.date.available	2015-06-03T06:47:03Z
dc.date.issued	1995
dc.identifier.citation	Current Science. 69(9); 1995; 767-770.	en_US
dc.identifier.uri	http://irgu.unigoa.ac.in/drs/handle/unigoa/757
dc.description.abstract	The transition between garnet and spinel peridotites, caused by the reaction orthopyroxene + spinel = olivine + garnet, has been envisaged in the harzburgites of Indus Ophiolite Belt based on petrographic and geochemical studies. The reaction has been tested in the light of evidence available from phase equilibrium experiments on such transition.	en_US
dc.publisher	Current Science Association, Bangalore	en_US
dc.subject	Earth Science	en_US
dc.title	Evidence of garnet to spinel peridotite transition In the harzburgites of Indus ophiolite belt: An indication of their mantle origin	en_US
dc.type	Journal article	en_US
dc.identifier.impf	y