El paleokarst cuaternario de Alcubilla del Marqués (Soria).

  1. Ramos Martín, M. C.
  2. Alonso Gavilán, Gaspar
Journal:
Geogaceta

ISSN: 0213-683X

Year of publication: 1990

Issue: 9

Pages: 77-79

Type: Article

DIALNET GOOGLE SCHOLAR lock_openArias Montano editor

More publications in: Geogaceta

Abstract

The paleokarst of Alcubil[a 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

Data source: Dialnet