Zobrazeno 1 - 4
of 4
pro vyhledávání: '"Daniel Cajade-Pascual"'
Publikováno v:
Journal of Marine Science and Engineering, Vol 7, Iss 10, p 331 (2019)
During the last glaciation, thick nival and periglacial sediments buried large sectors of the NW coast of Spain. The sediments were mostly eroded by the rising sea level during the Holocene, but in several places they remain, forming sedimentary clif
Externí odkaz:
https://doaj.org/article/bc6270c5aae2456c8e875ce8c4687967
Publikováno v:
Environmental Earth Sciences. 82
Coastal areas are extremely sensitive to variations in environmental conditions. The interaction of marine and continental processes causes a high degree of dynamism, generating depositional formations of great value for palaeoenvironmental reconstru
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::aa4b0d51cf08e2ab00e85fa55a0cc4ac
https://doi.org/10.1007/s12665-023-10955-7
https://doi.org/10.1007/s12665-023-10955-7
The coast is very sensitive to variations in environmental conditions. The interaction of marine and continental processes causes a high dynamism, generating depositional formations with a high value for paleoenvironmental reconstruction. This work f
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9215bd2cd54e3d7d41b0324b059ce318
https://doi.org/10.21203/rs.3.rs-2383025/v1
https://doi.org/10.21203/rs.3.rs-2383025/v1
Publikováno v:
Journal of Marine Science and Engineering
Volume 7
Issue 10
Minerva. Repositorio Institucional de la Universidad de Santiago de Compostela
instname
Journal of Marine Science and Engineering, Vol 7, Iss 10, p 331 (2019)
Volume 7
Issue 10
Minerva. Repositorio Institucional de la Universidad de Santiago de Compostela
instname
Journal of Marine Science and Engineering, Vol 7, Iss 10, p 331 (2019)
During the last glaciation, thick nival and periglacial sediments buried large sectors of the NW coast of Spain. The sediments were mostly eroded by the rising sea level during the Holocene, but in several places they remain, forming sedimentary clif
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::44f2c85ffdc5254fc3fda597d7f59977