RT Journal Article
T1 Movimientos verticales de las fallas alpinas NE-SO del MacizoIbérico en la región de Lugo
A1 Martín González, Fidel
A1 Capote del Villar, Ramón
A1 Insúa Arévalo, Juan Miguel
A1 Martínez Díaz, José J.
AB The vertical component of the movement associated to a fault system striking NE-SW has been determine using geomorphic and structural observations. These faults are located in the Iberian Massif in the Lugo region. The results of both kind o f observations have coincided in characterising these faults as hinge and pivotal faults. Moreover, considering the different periods of time recorded by these methods, we can establish that these faults are Tertiary and it is very difficult to explain a previous origin because of the structure complexity and the coincidence of the measures. In addition, and according to the results obtained from this area, we believe that the measures taken from the geomorphic markers, can be used alone as reliable indicators of the vertical component in this kind of faults, especially in areas where there are no others indicators.
PB Sociedad Geológica de España.
SN 1576-5172
YR 2004
FD 2004
LK https://hdl.handle.net/20.500.14352/52533
UL https://hdl.handle.net/20.500.14352/52533
LA spa
DS Docta Complutense
RD 2 may 2024