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http://hdl.handle.net/2183/5954 Estudio geológico-sedimentario de las cuencas terciario-cuaternarias de Monforte de Lemos, Maceda y Quiroga
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Olmo Sanz, Andrés del
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Cadernos do Laboratorio Xeolóxico de Laxe, 1986, 10: 83-93 ISSN: 0213-4497
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Abstract
[Resumen] Las cuencas terciario-cuaternarias de Monforte de Lemas, Maceda y Quiroga están situadas en la Hoja Geológica E. 1 : 200.000 de ORENSE-VERIN (NO. de la Península Ibérica). Estas cuencas no forman parte de una cuenca de mayores dimensiones sino que son cuencas continentales individuales e independientes. Su relleno se ha realizado mediante sistemas deposicionales como abanicos aluviales y transportes en masa. La creación de estas cuencas y su control sedimentario está ligado posiblemente a la acción de fallas en dirección.
[Abstract] The Tertiary-Quaternary basins of Monforte de Lemos, Maceda y Quiroga a relocated in the Geological chart E.l: 200.000 of ORENSE-VERIN (NW. of Iberian Penínsule). These basins do not form a part of a bigger basin, but they are individual and indipendent continental basins. Their filling-in has been attained through, depositional system like alluvial fans and mass flows. The orlgln of these bassins and their sedimentary control is possibly related, with the action of strike-slipe faults
[Abstract] The Tertiary-Quaternary basins of Monforte de Lemos, Maceda y Quiroga a relocated in the Geological chart E.l: 200.000 of ORENSE-VERIN (NW. of Iberian Penínsule). These basins do not form a part of a bigger basin, but they are individual and indipendent continental basins. Their filling-in has been attained through, depositional system like alluvial fans and mass flows. The orlgln of these bassins and their sedimentary control is possibly related, with the action of strike-slipe faults