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Alcune brecce titonico-neocomiane della sponda occidentale del Lago di Garda


, : Alcune brecce titonico-neocomiane della sponda occidentale del Lago di Garda. Bollettino della Societa Geologica Italiana 84(1): 41-51

Breccias occur at different horizons in the Jurassic (Tithonian)-Cretaceous section exposed on the western shore of Lake Garda (northern Italy). Two different types are defined, one of which is a limestone breccia (Tithonian) produced by synsedimentary submarine erosion and sliding of previously compacted Tithonian sediments. The other is polygenic (Tithonian-lower Cretaceous), resulting from large-scale slumping of partially or totally compacted limestones. The polygenic breccia grades laterally into the Maiolica limestone. Stratigraphic gaps in the section correspond to two distinct cycles of denudation, one pre-Tithonian, the other Tithonian-Neocomian.

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