A model for the formation of ultramafic rocks in the crust:Peridotites of southern Spain and Northern Morocco

Please use this identifier to cite or link to this item: http://dspace.mediu.edu.my:8181/xmlui/handle/10261/2920

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DC Field	Value	Language
dc.creator	Sánchez Cela, Vicente	-
dc.creator	Aparicio, Alfredo	-
dc.date	2008-02-12T09:01:47Z	-
dc.date	2008-02-12T09:01:47Z	-
dc.date	1997	-
dc.date.accessioned	2017-01-31T01:00:06Z	-
dc.date.available	2017-01-31T01:00:06Z	-
dc.identifier	http://hdl.handle.net/10261/2920	-
dc.identifier.uri	http://dspace.mediu.edu.my:8181/xmlui/handle/10261/2920	-
dc.description	The peridotite and related rocks of southern Spain and Northern Morocco were formed through polyphase processes by sialic matter than, at different P-T conditions transformed sedimentary-epimetamorphic materials	-
dc.description	Peer reviewed	-
dc.format	537322 bytes	-
dc.format	application/pdf	-
dc.language	eng	-
dc.publisher	Academia de Ciencias Exactas, Físicas, Químicas y Naturales de Zaragoza	-
dc.relation	Revista Academia Ciencias Zaragoza	-
dc.relation	52, ,197-210	-
dc.rights	openAccess	-
dc.subject	ultramafic sedimentary materials	-
dc.title	A model for the formation of ultramafic rocks in the crust:Peridotites of southern Spain and Northern Morocco	-
dc.type	Artículo	-
Appears in Collections:	Digital Csic

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