Redirigiendo al acceso original de articulo en 19 segundos...
Inicio  /  Andean Geology  /  Vol: 39 Núm: 2 Par: 0 (2012)  /  Artículo
ARTÍCULO
TITULO

3D deformation in strike-slip systems: Analogue modelling and numerical restoration

Daniel González    
Luisa Pinto    
Matías Peña    
César Arriagada    

Resumen

Regional and local strike-slip systems in Chile are complex and pose interesting questions, such as theinteraction between strike-slip and reverse faults, how they evolve, and the relationship between shortening, rotationand uplift. Within this context, we developed a new analytical method based on analogue and numerical modellingapplied to 3D, pure and transtensional-transpressional strike-slip systems. Analogue modelling results indicate that inrestraining stepovers of strike-slip fault systems, where antiformal pop-up structures are usually formed, pre-existentbasement structures with a high angle to the main strike-slip fault will generate a higher rotation of blocks. However,when these structures are oriented at a high angle with respect to the main stress convergence vector, the rotation willbe less and therefore a higher tendency to uplift will be produced. These results were applied to NW- and SE-strikingbasement faults oblique to N-S mega-thrust faults in central Chile (32º-35ºS), for which we propose a simultaneousdevelopment based on the analogue model results. Moreover, we propose that strike-slip movement occurred on thrustfaults in central Chile. Furthermore, we performed a numerical restoration of an analogue experiment which modeleda pure strike-slip system, and concluded that the restoration is very sensitive to shortening data as well as to rotationaldata. These results are extremely important for future numerical and regional analysis of strike-slip systems.

 Artículos similares

       
 
Eugenio E. Veloso,Ryo Anma,Atsushi Yamaji     Pág. 3 - 16
The repeated north and southward migration of the Chile Triple junction, offshore the Peni­nsula de Taitao, is expected to have imposed contrasting stress fields in the forearc for the last 6 Ma because of changes in convergence direction and rate of sub... ver más
Revista: Andean Geology

 
Arne P. Willner,Peter P. Richter,Uwe Ring     Pág. 17 - 36
In the Coastal Cordillera of central Chile a coherently preserved architecture of a late Paleozoic accretionary prism is exposed at 36°-35°S in cióse spatial association with a neighbouring área at 34°-35°S, where it is strongly modified by post-accretio... ver más
Revista: Andean Geology

 
Veronica Herrera,Jose Cembrano,Viviana Olivares,Shoji Kojima,Gloria Arancibia    
The interplay between fluid transport and crustal deformation is fairly well known in theory; however, it has seldom been described in actual field examples. The structural, microstructural and microthermometric analysis of fault-vein networks spatially ... ver más
Revista: Andean Geology

 
Beatriz Olivares,Jose Cembrano,Francisco Herve,Gloria Lopez,David Prior     Pág. 39 - 52
Metamorphic units of different age and structural levels occur at Isla Diego de Almagro (51°30'S), where they are juxtaposed by the Seno Arcabuz Shear Zone (SASZ). The SASZ strikes NNW and exposes deeper structural levels to the west of it. The SASZ rock... ver más
Revista: Andean Geology

 
Uwe Altenberger,Roland Oberhänsli,Benita Putlitz,Klaus Wemmer     Pág. 65 - 81
Five Miocene intrusive complexes are located along the N-trending, nearly trench-parallel San Lorenzo-Balmaceda Lineament in southern Patagonia. These complexes are characterized by mildly alkaline to calc-alkaline magmatism. The deformation and kinemati... ver más
Revista: Andean Geology