Magmatismo alcalino tardicadomiense en la zona de Ossa Morena (Macizo Ibérico): Cartografía, petrografía y geoquímica preliminar del Macizo de Almendral

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Magmatismo.pdf (1.37 MB)

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1999

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http://hdl.handle.net/10272/10095

Abstract

The Almendral massif is located in the north-western branch of the Olivenza-Monesterio antiform (Ossa Morena Zone, Iberian Massif, Spain). The pluton is composed by gabbros, sienites and alkaline granites which define an alkaline/transitional association. This magmatism marks the transition between the Cadomian orogenic regime and the Pre-Hercynian intracontinental rift for this sector

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Ossa Morena Zone; Alkaline/transitional magmatism; Cadomian late-orogenic alkaline stage

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Geogaceta -- Nº 26, (1999)
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The license for this item is described as Atribución-NoComercial-SinDerivadas 3.0 España