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handle: 20.500.14352/8511 , 10272/20543 , 10261/270203 , 10261/341734
La asociación espacial y cinemática entre kink bands en rocas con foliación varisca y cabalgamientos alpinos en el basamento del Sistema Central, permiten deducir que los primeros tienen una edad cenozoica, y no varisca o tardivarisca. Sistemáticamente, la dirección de los ejes de los kinks es subparalela a los cabalgamientos. Se estudian tres afloramientos clave: El Cabalgamiento de Villares de Jadraque, el Cabalgamiento de Valdesotos y el Retrocabalgamiento de El Atazar.
QE1-996.5, Geodinámica, 2507 Geofísica, Geology, Sistema Central., Artículos, kink bands, Central System, Alpine thrusts, 2506 Geología, Sistema Central, Cabalgamientos Alpinos, Kink bands, Geología, cabalgamientos alpinos, alpine thrusts, 551.24(234.1)
QE1-996.5, Geodinámica, 2507 Geofísica, Geology, Sistema Central., Artículos, kink bands, Central System, Alpine thrusts, 2506 Geología, Sistema Central, Cabalgamientos Alpinos, Kink bands, Geología, cabalgamientos alpinos, alpine thrusts, 551.24(234.1)
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