Termotectonic controls of the locals mineralizations: A work hypothesis

The volumetric and morphological changes undergone by rock forming minerals due to their relative differencial thermal dilatation (contractional) coeficients arc described as mineralization emplacement control. This way, the contrasting thermal dilatation data for quartz and felspar are reviewed by...

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Detalles Bibliográficos
Autor principal:	Rossello, E.A.
Formato:	JOUR
Materias:	Mineralizations Ore emplacement Structural control Thermal expansion magmatism mineralization morphology ore body spatial distribution tectonics
Acceso en línea:	http://hdl.handle.net/20.500.12110/paper_01019082_v26_n3_p191_Rossello
Aporte de:	Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires

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