
handle: 10272/10095
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
Cadomian late-orogenic alkaline stage, Ossa Morena Zone, Alkaline/transitional magmatism
Cadomian late-orogenic alkaline stage, Ossa Morena Zone, Alkaline/transitional magmatism
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