RT Journal Article
T1 Oscilaciones eustáticas e implicaciones climáticas en el tránsitoNeógeno-Cuaternario en la isla de Sal (archipiélago de Cabo Verde)
A1 Dabrio, Cristino J.
A1 Zazo Cardeña, Caridad
A1 González Delgado, José Ángel
A1 Goy Goy, José Luis
A1 Cabero del Río, Ana
A1 Hillaire-Marcel, Claude
A1 Ortlieb, L.
A1 Civis Llovera, Jorge
A1 Bardaji, T.
AB Solution pipes interpreted as a cryptokarst separate large-scale cross-bedded megaforms of shallowmarinecalcarenites deposited at the Neogene-Quatemary transition in Cape Verde Islands. Thisimplies that depositional phases were followed by subaerial exposure of the cemented calcarenitesduring subsequent falls of sea level, and accumulation of unconsolidated eolianites which supporteda 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 aridificationof climate at the beginning oi the Quaternary and the increased supply of Saharan dust byTrade Winds.
PB Sociedad Geológica de España.
SN 1576-5172
YR 2006
FD 2006
LK https://hdl.handle.net/20.500.14352/49330
UL https://hdl.handle.net/20.500.14352/49330
LA spa
DS Docta Complutense
RD 5 may 2024