2026-06-08T01:03:19Zhttps://docta.ucm.es/rest/oai/requestoai:docta.ucm.es:20.500.14352/120042024-07-24T18:21:13Zcom_20.500.14352_14col_20.500.14352_15
Docta Complutense
author
Oyarzun Muñoz, Roberto
author
López García, José Ángel
author
Crespo Feo, María Elena
author
Lillo, Javier
2023-06-17T12:26:25Z
2023-06-17T12:26:25Z
2018-03
1437-3254 (Print) ; 1437-3262 (Online)
10.1007/s00531-017-1514-5
https://hdl.handle.net/20.500.14352/12004
https://link.springer.com/article/10.1007%2Fs00531-017-1514-5
https://link.springer.com/
The southern end of Genoveses Bay (Cala de Genoveses) in Almería (SE Spain) hosts one of the most spectacular examples in Europe of combined (from base to the top), ignimbrite, surge, and pumice-ash fall deposits, forming a world-class outcrop of pyroclastic rocks. At a regional scale, the volcanism that led to the formation of these rocks has to be understood in terms of the late Alpine tectonic evolution of the western Mediterranean.
eng
Neat stratigraphic and dynamic relationships between pyroclastic flow and ash-cloud surge deposits in the Cabo de Gata–Níjar Geopark, Almería, Spain
journal article
URL
https://docta.ucm.es/bitstreams/f1cb31aa-5693-4989-b68c-cd20a0fc5488/download
File
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application/pdf
Neat stratigraphic and dynamic.pdf
URL
https://docta.ucm.es/bitstreams/dcdfa1d1-521f-4dde-9c5d-93a3e57720a8/download
File
MD5
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text/plain
Neat stratigraphic and dynamic.pdf.txt