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Discussion: Sediment accumulation on top of the Andean orogenic wedge: Oligocene to late Miocene basins of the Eastern Cordillera, southern BoliviaDiscussion

2000; Geological Society of America; Volume: 112; Issue: 11 Linguagem: Inglês

10.1130/0016-7606(2000)112 2.0.co;2

1943-2674

Thierry Sempéré,

Geochemistry and Geologic Mapping

Research Article| November 01, 2000 Discussion: Sediment accumulation on top of the Andean orogenic wedge: Oligocene to late Miocene basins of the Eastern Cordillera, southern BoliviaDiscussion Thierry Sempere Thierry Sempere 1Institut de Recherche pour le Développement, apartado postal 18-1209, Lima 18, Peru Search for other works by this author on: GSW Google Scholar Author and Article Information Thierry Sempere 1Institut de Recherche pour le Développement, apartado postal 18-1209, Lima 18, Peru Publisher: Geological Society of America Received: 04 Feb 1999 Revision Received: 21 Sep 1999 Accepted: 29 Oct 1999 First Online: 01 Jun 2017 Online ISSN: 1943-2674 Print ISSN: 0016-7606 Geological Society of America GSA Bulletin (2000) 112 (11): 1752–1755. https://doi.org/10.1130/0016-7606(2000)112 2.0.CO;2 Article history Received: 04 Feb 1999 Revision Received: 21 Sep 1999 Accepted: 29 Oct 1999 First Online: 01 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Tools Icon Tools Get Permissions Search Site Citation Thierry Sempere; Discussion: Sediment accumulation on top of the Andean orogenic wedge: Oligocene to late Miocene basins of the Eastern Cordillera, southern BoliviaDiscussion. GSA Bulletin 2000;; 112 (11): 1752–1755. doi: https://doi.org/10.1130/0016-7606(2000)112 2.0.CO;2 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGSA Bulletin Search Advanced Search In the Tupiza area of southern Bolivia, Cenozoic strata are outstandingly exposed in five north-trending basins. Because they could yield important information on the local Andean tectonic development, these basins were independently studied by Hérail et al. (1996), by a German group (Tawackoli et al., 1996; Kley et al., 1997; Tawackoli, 1997), and by Horton (1998). Geological maps by Hérail et al. and by Kley et al. agree fairly well (Fig. 1), and both studies recognize that west-vergent contraction has been dominant. According to Hérail et al., the area is a thin-skinned... You do not have access to this content, please speak to your institutional administrator if you feel you should have access.