@article{10272/18098,
year = {1990},
url = {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},
abstract = {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).},
publisher = {Sociedad Geológica de España},
keywords = {Sedimentology},
keywords = {Paleokarst},
keywords = {Plio-Pleistocene},
keywords = {Soria},
keywords = {Duero Basin},
title = {El paleokarst cuaternario de Alcubilla del Marqués (Soria)},
title = {The Quaternary paleokarst of Alcubilla del Marqués (Soria)},
author = {Ràmos Martín, M. C. and Alonso Gavilán, G.},
}