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E. Malinverno

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Open access Sep 2026

ANATOMY OF AN UPPER ZANCLEAN MIXED SILICI-BIOCLASTIC TRANSGRESSIVE SYSTEM: THE ROLE OF HIGH-FREQUENCY EUSTASY AND TECTONIC SUBSIDENCE ON THE STRATAL ARCHITECTURE OF THE SPUNGONE SANDSTONE, EASTERN CENTRAL ITALY

 The upper Zanclean Spungone Sandstone records the onset of a major transgression along the western margin of the Periadriatic Basin, eastern central Italy, and comprises a 130 m-thick succession of shallow-marine strata characterized by a highly regular cyclical stratigraphy. Integrated analysis of both physical and b...

C. D. Di Celma, Michela Principi, A. Pitts et al. · 0 citations

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