L'evolution du magmatisme dans le geosynclinal dinarique au Mesozoique et au Cenozoique

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Abstract
The inner and outer zones of the Dinaric Alps of Yugoslavia are compared. With the exception of Triassic porphyrites and quartz porphyrites and small upper Cretaceous rhyolite masses, the outer zone has few igneous rocks. The inner zone, however, was the scene of more extensive magmatic activity, represented by lower and middle Triassic porphyrites, Jurassic gabbros, melanophyres, and diabases, Oligocene and Pliocene granodiorites, andesites, dacites, and quartz monzonites, and late Pliocene andesites, basalts, and leucite basalts.

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