2026-06-28T14:49:59Zhttps://docta.ucm.es/rest/oai/requestoai:docta.ucm.es:20.500.14352/359692024-07-22T14:01:29Zcom_20.500.14352_14col_20.500.14352_21
Docta Complutense
author
Bardají Azcárate, Teresa
author
Cabero, A.
author
Lario, J.
author
Zazo, Caridad
author
Silva, P.G
author
Goy Goy, José Luis
author
Dabrio González, Cristino José
editor
Barlow, Natasha
editor
Koehler, Rich
2023-06-19T15:57:14Z
2023-06-19T15:57:14Z
2014-05-03
http://dggs.alaska.gov/webpubs/dggs/gb/text/gb012.pdf
https://hdl.handle.net/20.500.14352/35969
http://dggs.alaska.gov/
Trying to decipher how palaeoseismic activity has influenced the altitudinal disposition of interglacial deposits is one of the main challenges that must be achieved in order to quantify relative sea-level changes between consecutive highstands. Likewise, identifying palaeoseismic features in an area with low instrumental seismic activity can implement the seismic record and contribute to better seismic hazard knowledge. In this sense, Cope basin (SE Spain) becomes a reference basin to undertake this kind of analysis, firstly because of excellent outcrop conditions and secondly because the sea-level record is undoubtedly conditioned here by both effects: climatically driven changes and local and regional seismotectonics.
eng
Coseismic VS climatic effects in the record of relative sea-level changes: an example from last interglacials in SE Spain.
book part
URL
https://docta.ucm.es/bitstreams/8981ec57-483c-4dc1-b246-60503e5e4610/download
File
MD5
8d0bb743f868ffe6c8c4d44b14ae2f1a
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application/pdf
2014 AC-1 Coseismic vs non-seismic IGCP588 Conference-Alaska.pdf
URL
https://docta.ucm.es/bitstreams/2e99e16b-99c7-44a3-be5b-b38001780543/download
File
MD5
6ac05cd11d753f55781b180b010cf3e1
42668
text/plain
2014 AC-1 Coseismic vs non-seismic IGCP588 Conference-Alaska.pdf.txt