Las deformaciones hercinianas tardías en la región de Santa María la Real de Nieva (Sistema Central Español)
1988; Issue: 5 Linguagem: Inglês
ISSN
2173-6545
AutoresF. Álvarez, Francisco González Lodeiro, Luis Miguel Martín Parra,
Tópico(s)Geological and Tectonic Studies in Latin America
ResumoThe precambrian and paleozoic materials of Santa Maria la Real de Nieva outcrop has been affected by two Hercynian shear systems which developed after the main deformation phases and the intrusion of the granite rocks. The first shear system is composed of subvertical, dipping noothwards, senestral wrench faults trending ENE-WSW. The second is a low-angle extensional system with the hanging wa// descending westwards.
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