Controles estructurales del magmatismo cenozoico en Torres del Paine, Andes del sur (51°10'S).
Tectonic controls and Cenozoic magmatism at the Torres del Paine, southern Andes (Chile, 51°10'S)
| dc.contributor | en-US | |
| dc.contributor | es-ES | |
| dc.creator | Altenberger, Uwe | |
| dc.creator | Oberhänsli, Roland | |
| dc.creator | Putlitz, Benita | |
| dc.creator | Wemmer, Klaus | |
| dc.date | 2010-06-29 | |
| dc.identifier | http://www.andeangeology.cl/index.php/revista1/article/view/V30n1-a05 | |
| dc.identifier | 10.5027/andgeoV30n1-a05 | |
| dc.description | Cinco complejos intrusivos se situan a lo largo del Lineamiento San Lorenzo-Balmaceda, que es paralelo a la fosa oceanica de la Patagonia meridional. Estos complejos se caracterizan por tener un magmatismo levemente alcalino a calcoalcalino. Se estudiaron la deformacion y la cinematica en el antepais del lacolito Torres del Paine dominado por granitoides (12±2Ma) para evaluar la influencia del campo de esfuerzos corticales pre- y synintrusivo en el emplazamiento del magma. La compresion y la transpresion produjeron un plegamiento en gran escala, con pliegue de longitud de onda de hasta 10 km, y un fallamiento del flysch cretacico y de filones de gabro alcalino. La edad (29,4±0,8 Ma) de los gabros apuntan a una edad maxima oligocena para el plegamiento regional. Ocurren fallas inversas y fallas de rumbo convergentes y sinistrales asi como tambien se conjugan las fallas inversas. El ascenso del magma fue paralelo a la zona de falla Lago Grey de rumbo NNW-SSE,y probablemente coincide con la interseccion fosil de la falla transformante oceanica Madre de Dios. La intrusion se correlaciona en el tiempo con un cambio de dinamica transpresional a transtensional documentada por un cambio cinematico de falla de rumbo sinistral convergente a divergente y, en el espacio, con una reorganizacion de la situacion tectonica de placas durante el Mioceno. Despues de la colision de la dorsal de Chile que separa las placa de Nazca y Antartica, la parte suroccidental de Sur America cambio desde una convergencia rapida oblicua de direccion ENE-WSW entre la placa de Nazca y la placa Sudamerica a una convergencia frontal lenta de direccion este-oeste entre las placas Antartica y Sudamerica. La divergencia observada entre el lineamiento San Lorenzo-Balmaceda y el aparente control del ascenso de magmas a traves de fallas de la corteza superior puede ser explicada intepretando al SLB como un posible sistema de rumbo de la corteza inferior a gran escala, y por la particion del cizalle entre la corteza inferior y la superior. | es-ES |
| dc.description | 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 kinematics in the foreland of the granitoid-dominated Torres del Paine laccolith (12±2 Ma) were studied in order to evaluate the influence of the pre- to syn-intrusive crustal stress field on magma emplacement. Compression and transpression led to large-scale folding, with fold wavelength of up to 10 km, and faulting of the Cretaceous flysch sedimentary rocks as well as alkaline gabbro sills. Geochronological data from folded gabbros point to an Oligocene minimum age for regional folding at 29.4±0.8 Ma. Reverse faults and convergent sinistral strike-slip faults occur as well as conjugate reverse faults. The shortening axes trend ENE- to E. These directions correlate with the oblique convergence between the Nazca- and the South America-plate. The magma ascent was parallel to the NNW-SSE striking Lago Grey-fault zone and probably coincides with the fossil intersection of the oceanic Madre de Dios transform fault. The intrusion correlates with a change from transpressional to transtensional dynamics as documented by a kinematic change from left-lateral convergent strike-slip faulting to left-lateral divergent strike-slip faulting. The changes in dynamics and kinematics correlate in time and space with a reorganisation of the plate tectonic situation during the Miocene. After the collision of the Chile ridge, separating the Nazca-plate from Antarctica, the situation in the south-western part of South America changed from rapid ENE-WSW-directed oblique convergence between the Nazca- and South America-plate, to an east-west-directed slow frontal convergence between the Antarctica and South America plates. The observed geometric divergence of the San Lorenzo-Balmaceda lineament and the apparent control of magma ascent through upper crustal faults may be explained by the interpretation of the SLB as a possible large-scale lower crustal strike slip zone and by shear partitioning from lower crust to upper crust. | en-US |
| dc.format | application/pdf | |
| dc.format | text/html | |
| dc.language | eng | |
| dc.publisher | Servicio Nacional de Geología y Minería | en-US |
| dc.relation | http://www.andeangeology.cl/index.php/revista1/article/view/V30n1-a05/549 | |
| dc.relation | http://www.andeangeology.cl/index.php/revista1/article/view/V30n1-a05/html | |
| dc.source | Andean Geology; Vol 30, No 1 (2003); 65-81 | es-ES |
| dc.source | Andean Geology; Vol 30, No 1 (2003); 65-81 | en-US |
| dc.source | 0718-7106 | |
| dc.source | 0718-7092 | |
| dc.title | Controles estructurales del magmatismo cenozoico en Torres del Paine, Andes del sur (51°10'S). | es-ES |
| dc.title | Tectonic controls and Cenozoic magmatism at the Torres del Paine, southern Andes (Chile, 51°10'S) | en-US |
| dc.type | info:eu-repo/semantics/article | |
| dc.type | info:eu-repo/semantics/publishedVersion | |
| dc.type | es-ES | |
| dc.type | en-US |
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Andean Geology
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