2026-06-28T04:56:33Zhttps://docta.ucm.es/rest/oai/requestoai:docta.ucm.es:20.500.14352/493302024-07-18T14:36:27Zcom_20.500.14352_14col_20.500.14352_15
Docta Complutense
author
Dabrio González, Cristino José
author
Zazo Cardeña , Caridad
author
González Delgado, José Ángel
author
Goy Goy, José Luis
author
Cabero del Río, Ana
author
Hillaire-Marcel, Claude
author
Ortlieb, L.
author
Civis Llovera, Jorge
author
Bardaji, T.
2023-06-20T09:23:51Z
2023-06-20T09:23:51Z
2006
1576-5172
https://hdl.handle.net/20.500.14352/49330
Solution pipes interpreted as a cryptokarst separate large-scale cross-bedded megaforms of shallowmarine
calcarenites deposited at the Neogene-Quatemary transition in Cape Verde Islands. This
implies that depositional phases were followed by subaerial exposure of the cemented calcarenites
during subsequent falls of sea level, and accumulation of unconsolidated eolianites which supported
a vegetal cover that promoted the cryptokarst. The process was repeated several times.
A widespread, more recent karstification with red silty clay filling of voids may represent the aridification
of climate at the beginning oi the Quaternary and the increased supply of Saharan dust by
Trade Winds.
spa
Oscilaciones eustáticas e implicaciones climáticas en el tránsito
Neógeno-Cuaternario en la isla de Sal (archipiélago de Cabo Verde)
journal article
URL
https://docta.ucm.es/bitstreams/8ce97717-130c-4351-9d3a-36b96585b526/download
File
MD5
9d5b2c2eafcba71fe39bbe42ec36f80f
905942
application/pdf
2006_2_Cryptokarst_Sal_GEOTEMASl.pdf
URL
https://docta.ucm.es/bitstreams/4c5cd404-4669-4abd-b6bf-1acbff5c492d/download
File
MD5
11ed382dc8008cb5cc7cc8171a0257e4
13716
text/plain
2006_2_Cryptokarst_Sal_GEOTEMASl.pdf.txt