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Fault controlled development of shallow hydrothermal systems, Southern Andes

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Figure

Figure 1-1. Fault types in the Earth’s crust. a) Reverse fault: the hanging wall block  moves up with respect to the footwall block
Figure  1-2.  Fault  zone  architecture.  a)  Simple-core  and  b)  Multiple-core  fault  zone  (modified from Faulkner et al., 2003)
Figure  1-5.  Ranges  of  electrical  resistivity  in  common  rocks  and  sediments  (after  Telford et al., 1990, Ward, 1990)
Figure  2-1. Sample preparation for optical  microscopy. a) Sampled were  marked in  the plane of interest
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