Backset lamination produced by supercritical backwash flows at the beachface-shoreface transition of a storm-dominated gravelly beach (middle Pleistocene, central Italy)-Reference-Cited by-同舟云学术

Backset lamination produced by supercritical backwash flows at the beachface-shoreface transition of a storm-dominated gravelly beach (middle Pleistocene, central Italy)

Published:2020-02 Issue: Volume:112 Page:103987
ISSN:0264-8172
Container-title:Marine and Petroleum Geology
language:en
Short-container-title:Marine and Petroleum Geology

Author:

Di Celma Claudio^ORCID,Pitts Alan^ORCID,Jablonská Danica^ORCID,Haynes John T.^ORCID

Funder

University Studies Educational Leave program at James Madison University

Publisher

Elsevier BV

Subject

Stratigraphy,Economic Geology,Geology,Geophysics,Oceanography

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4. The plio-pleistocene succession between Trigno and Fortore rivers (Molise and Apulia Apennines): stratigraphy and facies characteristics;Amorosi;Geoacta,2009

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