ROLE OF STRUCTURAL CONTROL IN DEFINING THE GEOTHERMAL SYSTEM(S) IN SOUTH-CENTRAL CHILE
The relation between the geothermal systems and fracture density (FD) is quite evident from the structural analysis. FD correlates very well with the surface geothermal manifestations, as well as with the recharge areas of these geothermal systems. An increase in the (secondary) permeability in the uppermost 200-300 m in the areas of relatively high FD values, considered in the conceptual model, is consistent with the lithology, structure and stratigraphy of the area. Although the lineaments scatter in a wide range, the absence of lineaments between N60°E and N100°E is noticeable, and is consistent with displacement and stress data (Lavenu and Cembrano, 1999; Cembrano et al., 2007; Lara and Cembrano, 2009) of the Liquiñe-Ofqui Fault Zone. This indicates that such lineaments, which represent fractures and faults, are the result of recent deformation, causing secondary permeability that facilitates the subsurface flow particularly in NW-SE and N-S directions.
References:
Cembrano, J., A. Lavenu, G. Yañez (coordinators), R. Riquelme, M. Garcia, G. González, G. Herail, 2007. In: T. Moreno, W. Gibbons (Eds), The Geology of Chile, The Geological Society, London, 147–178.
Cembrano, J., E. Schermer, A. Lavenu, A. Sanhueza, 2000. Tectonophysics 319: 129–149.
Cembrano, J., L. Lara, 2009. Tectonophysics 471: 96–113.
Lavenu, A., J. Cembrano, 1999. Journal of Structural Geology 21: 1669–1691.