El paleokarst cuaternario de Alcubilla del Marqués (Soria)

Thumbnail Image

Files

El-paleokarst.pdf (329.73 KB)

Publication date

1990

Authors

Advisors

Department

Research group

Center

Metrics

Google Scholar

Export

Research Projects

Organizational Units

Journal Issue

URI

http://hdl.handle.net/10272/18098

Abstract

The paleokarst of Alcubilla del Marqués (Soria) is a portion of karstic building which has been eliminated by erosion. During karstic active stage, carbonatic (stalactite, stalagmite, cave popcorn) and siliciclastic (fluvial bars) sediments were developed
El paleokarst de Alcubilla del Marqués, Soria, es una porción de una formación kárstica que ha sido eliminada por la erosión. Durante el periodo activo kárstico, se desarrollaron sedimentos carbonáticos (estalactita, estalagmita, coraloide), y siliciclásticos (barras fluviales).

Keywords

Sedimentology; Paleokarst; Plio-Pleistocene; Soria; Duero Basin

Unesco Subjects

Bibliographic citation

Collections

Geogaceta -- Nº 09, (1990)
Atribución-NoComercial-SinDerivadas 3.0 España
The license for this item is described as Atribución-NoComercial-SinDerivadas 3.0 España