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Espinacito Range

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Journal Article
Journal: Lithosphere
Publisher: GSW
Published: 23 March 2018
Lithosphere (2018) 10 (3): 366–391.
... subsidence of the Cacheuta basin was driven by tectonic shortening in the Cordillera Principal at ca. 20 Ma and the uplift of the Espinacito range (Cordillera Frontal) north of 32.5°S ( Alarcón and Pinto, 2015 ). The western side of the Cacheuta basin was apparently largely removed by cannibalization...
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Journal Article
Journal: AAPG Bulletin
Published: 01 November 1958
AAPG Bulletin (1958) 42 (11): 2670–2691.
...). From this point it turns east to form the most eastern range of the Andes; then south through the northeastern part of Mendoza, terminating near the transverse valley of Rio Diamante. The dominating crests of the Frontal Cordillera are not much lower than those of their neighbors in the Principal...
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Journal Article
Published: 01 September 2003
Journal of the Geological Society (2003) 160 (5): 687–701.
...% ( Kley et al . 1999 ). This includes the Santiago and Huallaga Belts (Sub-Andean Ranges) of Peru ( Mathalone & Montoya 1995 ), the Bolivian and northernmost Argentinian Sub-Andean Ranges ( Roeder 1988 ; Baby et al . 1992 ; Dunn et al . 1995 ), the Argentinian Precordillera ( Jordan et al . 1993...
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Journal Article
Journal: AAPG Bulletin
Published: 01 October 1944
AAPG Bulletin (1944) 28 (10): 1455–1484.
... of bentonite which are mined for use in drilling mud. It has a great lateral lithologic variation as well as range in thickness. Its sandstones, although of low average permeability due to their tuffaceous character, produce oil in the Cacheuta and Lunlunta fields, and have been shown to contain oil...
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Journal Article
Published: 01 December 2021
Journal of Paleontology (2021) 95 (S85): 1–55.
... ) assigned an Aalenian–Bajocian range for the species in Chile. The species was later identified by Tornquist ( 1898 ) in Bajocian outcrops from Paso del Espinacito (San Juan Province, Argentina), although flank costae show an anterior disruption according to the figured shell. The material studied...
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Series: AAPG Memoir
Published: 01 January 2004
DOI: 10.1306/M82813C3
EISBN: 9781629810485
... ). Three segments will be analyzed to address this problem and characterize the Andean thrust system: a segment across the Puna high plateau and the Sub-Andean Ranges (22–23°S), another across the highest Andes of San Juan and Mendoza (32°–33°S), and a segment across the Neuquén Basin between 37° and 39°S...
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Series: GSA Special Papers
Published: 01 July 2008
DOI: 10.1130/2008.442(14)
... ( Hardy, 1981 ; Lucas and Estep, 1999 ; González-León et al., 2005 ), are scattered in several ranges of northwestern Sonora. The most complete sections of the El Antimonio Group occur in the Sierra del Álamo and Sierra de Santa Rosa mountains (Fig. 1) . Other bivalve-bearing sections of the Sierra...
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