Sediment dispersal pathways in the Po coastal plain since the Last Glacial Maximum: Provenance signals of autogenic and eustatic forcing-Reference-Cited by-同舟云学术

Sediment dispersal pathways in the Po coastal plain since the Last Glacial Maximum: Provenance signals of autogenic and eustatic forcing

Published:2020-10-17 Issue:2 Volume:33 Page:1407-1428
ISSN:0950-091X
Container-title:Basin Research
language:en
Short-container-title:Basin Res

Author:

Tentori Daniel¹²^ORCID,Amorosi Alessandro³^ORCID,Milli Salvatore¹²^ORCID,Marsaglia Kathleen M.⁴^ORCID

Affiliation:

1. Dipartimento di Scienze della Terra SAPIENZA Università di Roma Roma Italy

2. Istituto di Geologia Ambientale e Geoingegneria (IGAG) Consiglio Nazionale delle Ricerche Venezia Italy

3. Dipartimento di Scienze Biologiche, Geologiche e Naturali Università di Bologna Bologna Italy

4. Department of Geological Sciences California State University Northridge Northridge CA USA

Publisher

Wiley

Subject

Geology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1111/bre.12519

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3. Three‐fold nature of coastal progradation during the Holocene eustatic highstand, Po Plain, Italy – close correspondence of stratal character with distribution patterns

4. Global sea‐level control on local parasequence architecture from the Holocene record of the Po Plain, Italy;Amorosi A.;Marine and Petroleum Geology,2017

5. Paleosols and associated channel‐belt sand bodies from a continuously subsiding late Quaternary system (Po Basin, Italy): New insights into continental sequence stratigraphy;Amorosi A.;Bulletin,2017

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