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On the origin of the calciturbidites in the Tortonian hemipelagic marls of the Latium-Abruzzi carbonate platform domain (Central Apennines, Italy); tectonic, sea level changes or internal waves?

Crossref DOI link: https://doi.org/10.1007/s10347-025-00700-w

Published Online: 2025-04-01

Published Print: 2025-05

Update policy: https://doi.org/10.1007/springer_crossmark_policy

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