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Cerro Condor

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Journal Article
Journal: Palynology
Published: 01 November 2015
Palynology (2015) 39 (3): 362–386.
... Caracoles sections, Cerro Cóndor Depocentre Chubut province, northwestern Patagonia, Argentina is presented. The quantitative composition of the palynofloras is characterised by the dominance of pollen produced by the conifer families Cheirolepidiaceae ( Classopollis ) and Araucariaceae (mainly...
FIGURES | View All (11)
Series: GSA Engineering Geology Case Histories
Published: 01 January 1964
DOI: 10.1130/Eng-Case-5.1
EISBN: 9780813759302
Series: AAPG Studies in Geology
Published: 01 January 2008
EISBN: 9781629810331
... and story sets ( Figure 2C ). A channel story consists of a relatively conformable Outcrop Summary Condor West channel Location Specifics Parque Nacional Torres del Paine Country chile Formation Cerro Toro Age Late Cretaceous (Cenomanian to Campanian [∼74–97 Ma...
FIGURES
Series: AAPG Studies in Geology
Published: 01 January 2008
EISBN: 9781629810331
... Abstract The Condor channel complex, part of the Campanian Cerro Toro Formation (see overview by Fildani et al., chapter 32, this volume) forms part of an extensive outcrop belt exposed in the Pare Nacional Torres Del Paine in southern chile. The data presented here illustrate large, coarse...
Series: SEPM Field Trip Guidebook
Published: 01 January 2009
DOI: 10.2110/sepmfg.10.031
EISBN: 9781565762923
... . Figure 6.1. (A) Geologic map of Sierra del Toro, showing three discrete channel complexes that young to the east. The Condor complex (brown) contains the oldest Cerro Toro Formation channel deposits found at this location. The locations of outcrops featured in Figs. 6.1C and 6.2 are indicated...
FIGURES
Journal Article
Published: 01 December 2010
Journal of Sedimentary Research (2010) 80 (12): 1085–1108.
... deposits thinning onto both the eastern and western margins. The eastern margin of the Condor can be seen; however, the Guanaco is not present on the south side of Sierra del Toro. First mapped in the early twentieth century ( Hauthal 1907 ), the conglomeratic lenses of the Cerro Toro Formation...
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Journal Article
Journal: Economic Geology
Published: 01 March 2014
Economic Geology (2014) 109 (2): 487–502.
...Jaime A. Poblete; Thomas Bissig; James K. Mortensen; Janet Gabites; Richard Friedman; Manuel Rodriguez Abstract The Cerro Bayo low sulfidation epithermal district is located in the Aysén region, Chilean Patagonia, at the western tip of the Deseado Massif epithermal silver-gold province...
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Journal Article
Journal: Economic Geology
Published: 01 August 2016
Economic Geology (2016) 111 (5): 1043–1072.
...Stephen Leary; Richard H. Sillitoe; Peter W. Stewart; Karl J. Roa; Benjamin E. Nicolson Abstract Fruta del Norte is a completely concealed and extraordinarily well preserved epithermal gold-silver deposit located in the remote Cordillera del Cóndor mountain ranges of southeastern Ecuador. Currently...
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Image
Plan view of the major veins in the Rosario-<b>Cerro</b> La Grande area. Colored z...
Published: 01 August 2005
F ig . 14. Plan view of the major veins in the Rosario-Cerro La Grande area. Colored zones highlight the distribution of base and precious metals. Enargite-bearing veins with low Ag/Au occur at Cerro La Grande. Tennantite veins with high Ag/Au occur in the north and east at Rosario
Series: SEPM Field Trip Guidebook
Published: 01 January 2009
DOI: 10.2110/sepmfg.10.035
EISBN: 9781565762923
... Cerro Toro Formation channel complexes that young to the east, including ‘Condor’, ‘Guanaco’, and ‘Wildcat’. Arrows denote location of (B) and (C), photos of the north and south facies of the mountain respectively; also shown are locations of photos in Figs. 7.2 and 7.3 . (B) Conglomeratic deposits...
FIGURES
Journal Article
Journal: Economic Geology
Published: 01 August 2005
Economic Geology (2005) 100 (5): 835–862.
...F ig . 14. Plan view of the major veins in the Rosario-Cerro La Grande area. Colored zones highlight the distribution of base and precious metals. Enargite-bearing veins with low Ag/Au occur at Cerro La Grande. Tennantite veins with high Ag/Au occur in the north and east at Rosario...
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Image
Palaeoenvironmental scenario for the Early to Middle Jurassic of the Cañadó...
in > Palynology
Published: 01 November 2015
Figure 5 Palaeoenvironmental scenario for the Early to Middle Jurassic of the Cañadón Asfalto Formation, Cerro Cóndor depocentre, Chubut province, Argentina.
Series: GCSSEPM
Published: 01 December 2008
DOI: 10.5724/gcs.08.28.0268
EISBN: 978-0-9836096-2-9
.... Sedimentation style changed during deposition of the overlying Cerro Toro Formation (Coniacian-Campanian), which consists of thick successions of thin-bedded mudstone and sandstone turbidites and debris flow deposits interrupted by thick (up to 400 m) deep-water channel complexes. The channels are filled...
Journal Article
Published: 09 May 2008
Geological Magazine (2008) 145 (5): 714–732.
... number 56–59), coupled with very low incompatible element contents, flat LREE and fractionated HREE patterns (‘kinked’ pattern), and intermediate Sr–Nd–Pb isotope compositions. The Pleistocene basanites (Mg number 71–72) from the Cerro Ante monogenetic cone, on the easternmost slopes of the Patagonian...
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Image
Location of the outcrops of the Cañadón Asfalto Formation and the three sec...
in > Palynology
Published: 01 November 2015
Figure 1 Location of the outcrops of the Cañadón Asfalto Formation and the three sections (A, B and C) studied, Cerro Cóndor Depocentre, area of the middle Chubut River valley. Patagonia, Argentina. A: Cañadón Lahuincó ‘A’; B: Cañadón Lahuincó ‘B’ and C: Cañadón Caracoles.
Series: GSA Special Papers
Published: 01 January 2006
DOI: 10.1130/2006.2407(10)
...′W. CerroCondor,” 37°4.36′S, 68°53.18′W, 1450 ± 30 m at Base...
Journal Article
Journal: PALAIOS
Published: 01 September 2016
PALAIOS (2016) 31 (9): 405–420.
... it: Cerro Cóndor (middle Chubut River area), Fossati (Pampa de Gan Gan) ( Silva Nieto et al. 2007 ) and El Portezuelo-Llanquetrúz (NW of Gastre village) ( Figari et al. 1996 ). Our study corresponds to the Cerro Condor sub-basin, which has a large area and many outcrops with ample fossil records...
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Journal Article
Journal: Palynology
Published: 01 July 2015
Palynology (2015) 39 (2): 258–269.
... and the taphonomic effects with which they are associated, and to highlight the potential importance of their recognition. A full palynological study of the Cañadón Asfalto Formation from the Cerro Cóndor depocenter, Chubut province, forms part of the PhD thesis of Olivera (2012) . Pollen grains with fungal...
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Journal Article
Published: 24 May 2018
Journal of Paleontology (2018) 92 (6): 1054–1065.
... near the Lahuincó creek. This location is on the west side of the Chubut river, near provincial road No. 12 and 12 km south of the Cerro Condor village (43.30572°S, 69.8267°W). The original samples include a fossil association of conchostracans, bivalve mollusks, and ostracods. The material...
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Series: Geological Society, London, Special Publications
Published: 01 January 2015
DOI: 10.1144/SP399.5
EISBN: 9781862396753
... deformed by thrust propagation. South of the El Cóndor Creek, the bedrock topography rises from 850 m to 1000 m (on average) and defines the Cerros Colorados frontal range, which extends down to the southernmost exposures of the LPTS (Figs 2 & 3 , profile D–D′). A significant shortening...
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