El paleokarst cuaternario de Alcubilla del Marqués (Soria)
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
| Authors: | , |
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| Format: | article |
| Publication Date: | 1990 |
| Country: | España |
| Institution: | Universidad de Huelva (UHU) |
| Repository: | Arias Montano. Repositorio Institucional de la Universidad de Huelva |
| Language: | Spanish |
| OAI Identifier: | oai:ariasmontano.uhu.es:10272/18098 |
| Online Access: | http://hdl.handle.net/10272/18098 |
| Access Level: | Open access |
| Keyword: | Sedimentology Paleokarst Plio-Pleistocene Soria Duero Basin |
| Summary: | 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 |
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