Comparison of paleostress magnitudes from calcite twins with contemporary stress magnitudes and frictional sliding criteria in the continental crust: Mechanical implications

Author:

Lacombe Olivier

Publisher

Elsevier BV

Subject

Geology

Reference86 articles.

1. Rock Stress and Its Measurements,1997

2. Amrouch, K., Lacombe, O., Mouthereau, F., Dissez, L., 2005. Quantification of orientations and magnitudes of the late Cenozoic paleostresses in the Zagros folded belt from calcite twin analysis, in: Lacombe, O., Lavé, J., Roure, F. (convenors), Joint Earth Science Meeting SGF-SGE, Thrust belts and foreland basins, Rueil, Décembre 2005, Extended abstract volume, pp. 31–35.

3. The Dynamics of Faulting;Anderson,1951

4. A new method for the quantification of paleostress magnitudes: sequential sealing of the Soultz-sous-Forêt vein system (Rhine graben, France);André;Tectonophysics,2002

5. From orientation to magnitudes in paleostress determination using fault slip data;Angelier;J. Struct. Geol.,1989

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