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Publikováno v:
Marine Geology. 266:232-243
The ravinement surface is a key marker for examining the effects of the most recent sea-level transgression on development of the latest Pleistocene–Holocene stratigraphic record of the New Jersey middle and outer continental shelf. This surface is
Autor:
Laurie Schuur Duncan, John A. Goff
Publikováno v:
Sediments, Morphology and Sedimentary Processes on Continental Shelves
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d1eeb86f3be73a196a743a5edab657d0
https://doi.org/10.1002/9781118311172.ch6
https://doi.org/10.1002/9781118311172.ch6