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Fiambala Basin

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Journal Article
Journal: GSA Bulletin
Published: 01 November 2008
GSA Bulletin (2008) 120 (11-12): 1518-1543.
..., how such deformation styles influence sedimentation patterns, and whether or not broken foreland basins are related to regional plate-tectonic processes, such as flat-slab subduction. The Fiambalá basin of the northwestern Sierras Pampeanas is the largest of several intermontane basins...
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Journal Article
Journal: GSA Bulletin
Published: 01 May 2010
GSA Bulletin (2010) 122 (5-6): 946-949.
...Federico M. Dávila Figure 1. (A) Perspective view from above and to the NW of the Famatina geological province and boundary regions (Vinchina, Bermejo, and Puna). Note the Fiambalá Basin (location of Carrapa et al., 2008 ) in the northernmost part of Famatina. The central Famatina (location...
FIGURES
Journal Article
Journal: GSA Bulletin
Published: 01 May 2010
GSA Bulletin (2010) 122 (5-6): 950-953.
... at 6 Ma is a response to the peak of flat-slab shallowing. Figure 1. Satellite image of the southern-central Andes with location of the Neogene basins discussed in the text. The stratigraphy of the Bermejo Foreland basin is after Jordan et al. (2001) , of the Fiambalá basin from the present...
FIGURES
Series: GSA Memoirs
Published: 01 January 2015
DOI: 10.1130/2015.1212(10)
... in exhumation in the Precordillera and northern Sierras Pampeanas at the southeastern flank of the Puna Plateau at ~28°S. In this study, we mapped an ~80-km-wide transect at a latitude of ~28°S in the Sierra de Las Planchadas and the Fiambalá Basin. Apatite fission-track (AFT) ages from six samples from thrust...
Series: GSA Memoirs
Published: 01 January 2015
DOI: 10.1130/2015.1212(13)
... deposition along the margin of the Puna Plateau in the Fiambalá and El Cajon Basins. Combining this with existing data, we explore the relative roles of climate and tectonics in shaping sedimentation in this region. Our analysis reveals that Punaschotter deposition was diachronous and only occurred if both...
Series: AAPG Memoir
Published: 01 January 2003
DOI: 10.1306/M78834C2
EISBN: 9781629810539
...%, of the earth’s land surface. In this paper, we present maps showing the location of all 877 giants located on tectonic and sedimentary basin maps of these 27 key regions. We classify the tectonic setting of the giants in these regions using six simplified classes of the tectonic setting for basins...
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Journal Article
Journal: GSA Bulletin
Published: 01 January 2017
GSA Bulletin (2017) 129 (1-2): 152-170.
... , doi:10.1029/2004TC001762. Carrapa , B. , Strecker , M. , and Sobel , E. , 2006 , Cenozoic orogenic growth in the Central Andes: Evidence from sedimentary rock provenance and apatite fission track thermochronology in the Fiambalá Basin, southernmost Puna Plateau margin (NW Argentina...
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Journal Article
Published: 28 July 2016
Geological Magazine (2016) 153 (5-6): 926-944.
... 2016 Copyright © Cambridge University Press 2016 2016 Cambridge University Press tectonics cross-section Neuquén Basin structural inheritance kinematics The inversion of extensional sedimentary basins has received much attention during the last three decades due...
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Journal Article
Journal: GSA Bulletin
Published: 01 November 2014
GSA Bulletin (2014) 126 (11-12): 1439-1464.
...Clayton S. Painter; Barbara Carrapa; Peter G. DeCelles; George E. Gehrels; Stuart N. Thomson Abstract New low-temperature thermochronology and geochronology data from Upper Jurassic–Upper Cretaceous strata from the North American Cordilleran foreland basin in Utah, Colorado, Wyoming, and South...
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Journal Article
Journal: AAPG Bulletin
Published: 01 January 1987
AAPG Bulletin (1987) 71 (1): 49-64.
...Teresa E. Jordan; Ricardo N. Alonso ABSTRACT Clastic sedimentary basins have evolved during the past 40 m.y. in the central Andes (lat. 20°–28°S) in response to shifting patterns of magmatism and deformation. The distribution of these basins and their genetic relations to uplifted areas...
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Journal Article
Journal: Lithosphere
Published: 01 June 2015
Lithosphere (2015) 7 (3): 336-352.
... rapid exhumation at ca. 21–14 Ma in the Cerro Negro ( Carrapa et al., 2014 ). This exhumation is also recorded by detrital apatite fission-track data in sediments preserved in the Fiambalá basin (Fia, Fig. 3 ) with a strong 14 Ma signal, suggesting the southern margin of the Puna Plateau was exhuming...
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Image
(A) Perspective view from above and to the NW of the Famatina geological pr...
Published: 01 May 2010
Figure 1. (A) Perspective view from above and to the NW of the Famatina geological province and boundary regions (Vinchina, Bermejo, and Puna). Note the Fiambalá Basin (location of Carrapa et al., 2008 ) in the northernmost part of Famatina. The central Famatina (location of Dávila and Astini
Journal Article
Published: 20 August 2000
Canadian Journal of Earth Sciences (2001) 38 (8): 1263-1283.
...Blas L. Valero-Garcés; Concha Arenas; Antonio Delgado-Huertas Abstract Four distinctive depositional subenvironments of fossil travertines and stromatolites are identified in three high-altitude (3500–4000 m above sea level) lacustrine basins: El Peinado, San Francisco (Las Coladas Salar subbasin...
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Journal Article
Journal: GSA Bulletin
Published: 01 January 2014
GSA Bulletin (2014) 126 (1-2): 66-77.
..., providing clastic material to the El Cajon and Santa Maria Basins ( Sobel and Strecker, 2003 ; Mortimer et al., 2007 ). Farther to the south, the Sierras Pampeanas mainly preserves a variety of Cenozoic and pre-Cenozoic ages. Detrital AFT ages from the Fiambalá Basin fill at ∼28°S record a strong mid...
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Image
(A) Digital elevation model (DEM) of the study area and morphotectonic doma...
Published: 01 November 2008
Figure 1. (A) Digital elevation model (DEM) of the study area and morphotectonic domains (shown on inset map) (modified after Jordan et al., 1983 ; Isacks, 1988 ). White line corresponds to the area of the Puna Plateau characterized by internal drainage. (B) Geological map of the Fiambalá basin
Journal Article
Journal: Geology
Published: 01 July 2009
Geology (2009) 37 (7): 643-646.
...., 2007 ). At ~28°S, the Bolsón de Fiambala ( Fig. 1 ) records a broken foreland after 6 Ma ago, and reduced fluvial connectivity by 3.7 Ma ago ( Carrapa et al., 2008 ). Nonsystematic basin fragmentation east of the Puna suggests that the plateau has not been growing laterally through progressive...
FIGURES
Image
Satellite image of the southern-central Andes with location of the Neogene ...
Published: 01 May 2010
Figure 1. Satellite image of the southern-central Andes with location of the Neogene basins discussed in the text. The stratigraphy of the Bermejo Foreland basin is after Jordan et al. (2001) , of the Fiambalá basin from the present work, of the Corral Quemado basin after Muruaga (2001
Image
Satellite image of the southern Central Andes and location of the Neogene b...
Published: 01 November 2008
Figure 13. Satellite image of the southern Central Andes and location of the Neogene basins discussed in the text. The stratigraphy of the Bermejo foreland basin is after Jordan et al. (2001) , the Fiambalá basin stratigraphy is from the present work, Corral Quemado basin stratigraphy is after
Journal Article
Journal: Geology
Published: 07 June 2018
Geology (2018) 46 (7): 647-650.
... , E. , 2006 , Cenozoic orogenic growth in the Central Andes: Evidence from sedimentary rock provenance and apatite fission track thermochronology in the Fiambalá Basin, southernmost Puna Plateau margin (NW Argentina) : Earth and Planetary Science Letters , v. 247 , p. 82 – 100 , https...
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Series: Geological Society, London, Special Publications
Published: 01 January 2005
DOI: 10.1144/GSL.SP.2005.246.01.08
EISBN: 9781862394940
...-arc basin. The Las Termas belt is suggested as representing remnants of this back- arc basin. The varied and unusual rock series around the thermal springs of Fiambalá north of Tinogasta ( Fig. 2 ) and the ‘Fiambalá meta- gabbronorite (FMGN)’, a meta-igneous body of about 13 × 0.4 km, elongated...
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