Análisis tensorial de la deformación superpuesta en el límite oriental de la cuenca de Madrid
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Análisis tensorial de la deformación superpuesta en el límite oriental de la cuenca de MadridTítulo(s) alternativo(s)
Tensorial analisis of the superposed deformation in the easthern border of the Madrid basinData
1994Cita bibliográfica
Cadernos do Laboratorio Xeolóxico de Laxe, 1994, 19: 203-214 ISSN: 0213-4497
Resumo
An analysis of Neogene brittle deformation using fault populatíon analysis methods has been carried out between the SW border of the Iberian Range and Altomira Range. Two main paleostress fields have been established: 1) N70E - N120E compression (Altomira paleostress field) ofLate Oligocene - Early Miocene age that induced the formation of the SW border of Iberian Range and Altomira - Pareja thrust belts with reverse and strike-slip faults.
2) N140-N160E compression (Guadarrama paleostress field) of Middle Aragonian - early Pleistocene age that reactivated previous faults with strikeslip movement along the Iberian Range. A superposition of two regional stress fields (Iberian and Guadarrama) is proposed to explain E-W compression that formed Altomira Range. Stress tensorial additions have been realized to check this hypothesis.
Palabras chave
Altomira Range
Neogene
Brittle deformation
Fault population analysis
Stress tensor
Paleostress field
Neogene
Brittle deformation
Fault population analysis
Stress tensor
Paleostress field
ISSN
0213-4497