dc.contributor.author | Elger, Kirsten | |
dc.date.accessioned | 2010-10-28T18:46:41Z | |
dc.date.available | 2010-10-28T18:46:41Z | |
dc.date.issued | 2004 | |
dc.identifier.uri | http://hdl.handle.net/11858/00-1735-0000-0001-32E2-9 | |
dc.identifier.uri | http://doi.org/10.2312/GFZ.B103-03052 | |
dc.description.abstract | The Altiplano represents a key region of the Central Andes, where the interplay between faults and syn-tectonic sediments allow the reconstruction of the kinematic evolution of the Central Andean high plateau. This study aims, by the use of incrementally-balanced crosssections, interpretation of reflection-seismic profiles, 3D strain analysis, gravity data interpretation, isotopic-age dating, and surface observations, to reconstruct the geological and tectonic history of the Southern Altiplano at 21o S between the Eastern and the Western Cordillera. The Southern Altiplano is a complex intramontane basin with 6-8km Cenozoic fill. It can be structurally divided in three domains; the Eastern, Central, and Western Altiplano. 2D balanced cross-sections based on seismic-reflector analysis and field observations show that the Eastern Altiplano is the buried, thin-skinned deformation front of the western part of the Eastern Cordillera's bivergent thrust system. The 20-40ʿ dipping, blind faults merge into a shallow, eastward-dipping detachment at 7-9km depth that continues into the Eastern Cordillera. The Central Altiplano forms a bivergent system with 30-90ʿ dipping, basement-involving thrusts in the east, and fault-propagation folds in the west. The shallow, westward-dipping detachment lies at 9-10km depth and possibly continues into the Western Altiplano, which forms a separate bivergent thrust-system.The computer-aided (GeoSec and 2DMove), incremental restoration of the balanced crosssections of the Eastern and Central Altiplano, and preliminary line-length balancing of the Western Altiplano, yields 38km shortening due to folding and thrusting ... | |
dc.format.mimetype | application/pdf | |
dc.language.iso | eng | |
dc.publisher | GFZ, Helmholtz-Zentrum | |
dc.rights.uri | http://creativecommons.org/licenses/by-nc-sa/3.0/de/deed.de | |
dc.subject.ddc | 551 | |
dc.subject.gok | VAE 811 | |
dc.subject.gok | TQC 220 | |
dc.subject.gok | VEX 300 | |
dc.subject.gok | VEX 100 | |
dc.title | Analysis of deformation and tectonic history of the Southern Altiplano Plateau (Bolivia) and their importance for plateau formation | |
dc.type | monograph | |
dc.subject.gokverbal | Alpidische Orogene {Geologie} | |
dc.subject.gokverbal | Reflexionsseismik {Geophysik} | |
dc.subject.gokverbal | Bolivien und Paraguay {Geologie} | |
dc.subject.gokverbal | Anden {Geologie} | |
dc.identifier.doi | 10.2312/GFZ.B103-03052 | |
dc.identifier.ppn | 390991031 | |
dc.type.version | publishedVersion | |
dc.relation.volume | Scientific Technical Report / Geoforschungszentrum Potsdam; 2003, 05 | |
dc.bibliographicCitation.journal | Scientific Technical Report / Geoforschungszentrum Potsdam | |
dc.relation.collection | Geophysik | |
dc.description.type | thesis | |