Pregled bibliografske jedinice broj: 816710
Caracterización de la geometría de la depresión de Navamuño (Sistema Central Español) aplicando técnicas geofísicas
Caracterización de la geometría de la depresión de Navamuño (Sistema Central Español) aplicando técnicas geofísicas // Geogaceta, 57 (2015), 39-42 (podatak o recenziji nije dostupan, članak, znanstveni)
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Naslov
Caracterización de la geometría de la depresión de Navamuño (Sistema Central Español) aplicando técnicas geofísicas
(Characterization of the geometry of the Navamuño depression (Spanish Central System) by using geophysical techniques)
Autori
Rosa M., Carrasco ; Jesús, Sánchez ; Alfonso, Muñoz Martín ; Javier, Pedraza ; Antonio J., Olaiz ; Blanca, Ruiz Zapata ; Daniel, Abel-Schaad ; Oscar, Merlo ; David, Domínguez-Villar
Izvornik
Geogaceta (0213-683X) 57
(2015);
39-42
Vrsta, podvrsta i kategorija rada
Radovi u časopisima, članak, znanstveni
Ključne riječi
Depresión tipo nava ; tomografía de resistividad eléctrica TRE) ; sondeos eléctricos verticales (SEV) ; morfotectónica ; Sistema Central Español
(Pseudoendorheic depression ; electrical resistivity tomography (ERT) ; vertical electric sounding (VES) ; morphotectonic ; Spanish Central System)
Sažetak
The Navamuño depression, located in the high sector of the Cuerpo de Hombre valley (Sierra de Béjar), was partly occupied by a glacier during the Late Pleistocene. The basin is a ~14 Ha pseudoendorheic depression with boundaries defined by fault lineaments and the left lateral moraine of the Cuerpo de Hombre paleoglacier. The geometry of the base of the basin and the thickness of sediments that contain were studied together with the relationship of these deposits with the structural elements. Eight bi-dimensional profiles of electrical resistivity tomography were carried out supported by nine vertical electrical sounding logs. Although heterogeneous, the maximum thickness of the deposit infilling the basin is higher than approximately 20 m in some sectors, with three units under the urficial soil. The depression is interpreted as a basin filled with fluvioglaciar and fluviotorrential deposits with episodes of local shallow pond/bog peat sedimentation.
Izvorni jezik
Spa
Znanstvena područja
Geologija