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José Meulen Piquer Romo,Gonzalo Yáñez,Orlando Rivera,David Cooke
Pág. 223 - 239
Long-lived, high-angle fault systems constitute high-permeability zones that can localize the upward flow of hydrothermal fluids and magma throughout the upper crust. Intersections of these types of structures can develop complex interference patterns, w...
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