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http://hdl.handle.net/2183/6346 Estratigrafía de la margen izquierda de la Cuenca de Meirama
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Caravantes, P. A.
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Cadernos do Laboratorio Xeolóxico de Laxe, 1983, 6: 189-201 ISBN: 84-7492-204-6
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Abstract
[Resumen] Se describen unos materiales situados en la margen izquierda de la cuenca lignitífera de Meirama. Su génesis está controlada por subsidencia diferencial, motivada seguramente por dos fallas transversales al valle y que hacen que el conjunto dé una disposición en discordancia progresiva. Los sedimentos formados por materiales detríticos, unas veces carbonosos y otras no, indican la coexistencia de dos medios: el paludial y el aluvial
[Abstract] Are described the materials located in the 1eft margin of lignitiferous basin of Meirama. Your génesis was controlled by differential sinking, possibly related with two transverse faults, to the main valley direction, that lead the upper sedimentary unit underwent a progressive discordance. The sediments are detrita1, carbonaceous or not, showing the coexistence of paludial and aluvial deposition medium.
[Abstract] Are described the materials located in the 1eft margin of lignitiferous basin of Meirama. Your génesis was controlled by differential sinking, possibly related with two transverse faults, to the main valley direction, that lead the upper sedimentary unit underwent a progressive discordance. The sediments are detrita1, carbonaceous or not, showing the coexistence of paludial and aluvial deposition medium.