Artigo Revisado por pares

Unroofing the core of the central Andean fold-thrust belt during focused late Miocene exhumation: evidence from the Tipuani-Mapiri wedge-top basin, Bolivia

2010; Wiley; Volume: 23; Issue: 3 Linguagem: Inglês

10.1111/j.1365-2117.2010.00491.x

ISSN

1365-2117

Autores

J.G. Mosolf, Brian K. Horton, Matthew T. Heizler, Ramiro Matos,

Tópico(s)

earthquake and tectonic studies

Resumo

Basin ResearchVolume 23, Issue 3 p. 346-360 Unroofing the core of the central Andean fold-thrust belt during focused late Miocene exhumation: evidence from the Tipuani-Mapiri wedge-top basin, Bolivia Jesse G. Mosolf, Jesse G. Mosolf Department of Earth Science, University of California, Santa Barbara, CA, USASearch for more papers by this authorBrian K. Horton, Brian K. Horton Institute for Geophysics and Department of Geological Sciences, Jackson School of Geosciences, University of Texas at Austin, Austin, TX, USASearch for more papers by this authorMatthew T. Heizler, Matthew T. Heizler New Mexico Bureau of Geology and Mineral Resources, Socorro, NM, USASearch for more papers by this authorRamiro Matos, Ramiro Matos Instituto de Investigaciones Geológicas y Medio Ambiente, Universidad Mayor de San Andrés, La Paz, BoliviaSearch for more papers by this author Jesse G. Mosolf, Jesse G. Mosolf Department of Earth Science, University of California, Santa Barbara, CA, USASearch for more papers by this authorBrian K. Horton, Brian K. Horton Institute for Geophysics and Department of Geological Sciences, Jackson School of Geosciences, University of Texas at Austin, Austin, TX, USASearch for more papers by this authorMatthew T. Heizler, Matthew T. Heizler New Mexico Bureau of Geology and Mineral Resources, Socorro, NM, USASearch for more papers by this authorRamiro Matos, Ramiro Matos Instituto de Investigaciones Geológicas y Medio Ambiente, Universidad Mayor de San Andrés, La Paz, BoliviaSearch for more papers by this author First published: 21 October 2010 https://doi.org/10.1111/j.1365-2117.2010.00491.xCitations: 17 Jesse G. Mosolf, Department of Earth Science, University of California, Santa Barbara, CA 93106-9630, USA. E-mail: [email protected] Read the full textAboutPDF ToolsRequest permissionExport citationAdd to favoritesTrack citation ShareShare Give accessShare full text accessShare full-text accessPlease review our Terms and Conditions of Use and check box below to share full-text version of article.I have read and accept the Wiley Online Library Terms and Conditions of UseShareable LinkUse the link below to share a full-text version of this article with your friends and colleagues. Learn more.Copy URL Share a linkShare onEmailFacebookTwitterLinkedInRedditWechat ABSTRACT As the highest part of the central Andean fold-thrust belt, the Eastern Cordillera defines an orographic barrier dividing the Altiplano hinterland from the South American foreland. Although the Eastern Cordillera influences the climatic and geomorphic evolution of the central Andes, the interplay among tectonics, climate and erosion remains unclear. We investigate these relationships through analyses of the depositional systems, sediment provenance and 40Ar/39Ar geochronology of the upper Miocene Cangalli Formation exposed in the Tipuani-Mapiri basin (15–16°S) along the boundary of the Eastern Cordillera and Interandean Zone in Bolivia. Results indicate that coarse-grained nonmarine sediments accumulated in a wedge-top basin upon a palaeotopographic surface deeply incised into deformed Palaeozoic rocks. Seven lithofacies and three lithofacies associations reflect deposition by high-energy braided river systems, with stratigraphic relationships revealing significant (∼500 m) palaeorelief. Palaeocurrents and compositional provenance data link sediment accumulation to pronounced late Miocene erosion of the deepest levels of the Eastern Cordillera. 40Ar/39Ar ages of interbedded tuffs suggest that sedimentation along the Eastern Cordillera–Interandean Zone boundary was ongoing by 9.2 Ma and continued until at least ∼7.4 Ma. Limited deformation of subhorizontal basin fill, in comparison with folded and faulted rocks of the unconformably underlying Palaeozoic section, implies that the thrust front had advanced into the Subandean Zone by the 11–9 Ma onset of basin filling. Documented rapid exhumation of the Eastern Cordillera from ∼11 Ma onward was decoupled from upper-crustal shortening and coeval with sedimentation in the Tipuani-Mapiri basin, suggesting climate change (enhanced precipitation) or lower crustal and mantle processes (stacking of basement thrust sheets or removal of mantle lithosphere) as possible controls on late Cenozoic erosion and wedge-top accumulation. Regardless of the precise trigger, we propose that an abruptly increased supply of wedge-top sediment produced an additional sedimentary load that helped promote late Miocene advance of the central Andean thrust front in the Subandean Zone. Supporting Information Table S1. 40Ar/39Ar analytical data. 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