María del Carmen García Cuevas, José Manuel González Casado, Gerardo de Vicente Muñoz
The twinned-calcite strain-gauge technique allows determination of main axis strain magnitudes and orientations in limestones rocks midly deformed (Groshong, 1972), during Alpine orogeny in the lberian Chain. This estudy combinates calcite twin analysis with fault analysis. The calculated paleostrain and paleostress tensor have similar characteristics and a good correlation have been established between these two procedures.
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