TR method (TRM): A separation and stress inversion method for heterogeneous fault-slip data driven by Andersonian extensional and compressional stress regimes
Author:
Publisher
Elsevier BV
Subject
Geology
Reference71 articles.
1. The dynamics of faulting;Anderson;Trans. Edinb. Geol. Soc.,1905
2. The Dynamics of Faulting;Anderson,1951
3. Determination of the mean principal directions of stresses for a given fault population;Angelier;Tectonophysics,1979
4. Tectonic analysis of fault-slip data sets;Angelier;J. Geophys. Res.,1984
5. From orientation to magnitudes in paleostress determinations using fault slip data;Angelier;J. Struct. Geol.,1989
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