Ley de distribución de planos de debilidad en la Sierra de Atapuerca (Burgos): aplicación al drenaje del karst
In this work, we apply a method, which has been widely verified, of the study and use of the microtectonic data gathered in the field (parameters used are strike, dip and sense of dip of tectoglyphs: stylolite plans, mineral veins and fault plans), for analysis and quantification of the directional...
| Autores: | , , , , , , , |
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| Tipo de recurso: | artículo |
| Fecha de publicación: | 1997 |
| País: | España |
| Institución: | Universidad de Huelva (UHU) |
| Repositorio: | Arias Montano. Repositorio Institucional de la Universidad de Huelva |
| Idioma: | español |
| OAI Identifier: | oai:ariasmontano.uhu.es:10272/10454 |
| Acceso en línea: | http://hdl.handle.net/10272/10454 |
| Access Level: | acceso abierto |
| Palabra clave: | Karst Distribution law Endorrhehic drainage Atapuerca |
| Sumario: | In this work, we apply a method, which has been widely verified, of the study and use of the microtectonic data gathered in the field (parameters used are strike, dip and sense of dip of tectoglyphs: stylolite plans, mineral veins and fault plans), for analysis and quantification of the directional anisotropy in the lime outcrop of Atapuerca. We obtain four main drainage directions: N 7 7 7°-120°, N 93°, N 756° and N 6° with 14,8%, TO,9% , 7 0,8% and 8,6% probabilitys respectively. Each with its own normal distributions overlaping to themselves. The contrast of the drainage prediction and conduit directions polimodals shows that the maximum error between prediction modes and the found in the direction of the caves is 3,9% |
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