Significado paleogeográfico de las texturas y acumulaciones de carbonatos en perfiles edáficos de la Unidad Intermedia del Mioceno de la Cuenca de Madrid (prov. de Guadalajara)
- Ana María Alonso-Zarza 1
- María Ángeles García del Cura 1
- José Pedro Calvo Sorando 1
- 1 Geociencias. Medio-Ambiente
ISSN: 0213-683X
Año de publicación: 1988
Número: 5
Páginas: 29-33
Tipo: Artículo
Otras publicaciones en: Geogaceta
Resumen
The presence as well as types of pedogenic carbonate deposits within miocene formations of the NE Madrid Basin are mainly linked to two majar differentitated environments: a) proximal alluvial fan environments and b) distal alluvial fan and flood-plain environments. The pedogenic profiles developed in palustrine areas show sorne features a/so found in b) deposits. In a broad sense, both mesoscale and textura/ features (Fe-Mn oxides remobilization and carbonate accumulation) of the pedogenic profiles display sorne variety resulting from different sedimentation rates, substrate nature and water hosting, al/ the parameters being controlled by pa/eogeography.