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Rancho Los Chinos Mexico

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Series: GSA Special Papers
Published: 01 July 2008
DOI: 10.1130/2008.442(05)
... continental shelf (Rancho Placeritos), and offshelf continental rise (Rancho Los Chinos). Ages of Devonian brachiopod faunas include middle Early (Pragian) at Rancho Placeritos in west-central Sonora, late Middle (Givetian) at Cerros de Los Murciélagos in northwestern Sonora, and late Late (Famennian...
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Series: GSA Special Papers
Published: 01 July 2008
DOI: 10.1130/2008.442(08)
...-rise Los Pozos conglomeratic barite sandstone and the foredeep Mina México calciclastic sandstone imply different depositional and tectonic settings. Ages of detrital zircons in Paleozoic sandstones of northwestern Mexico provide information for locating source terranes...
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Series: GSA Special Papers
Published: 01 January 2007
DOI: 10.1130/2007.2422(07)
... of NW México and SW Arizona (modified after Molina Garza and Geissman, 1998 ). Abbreviations for localities: SLT—Sierra Los Tanques; QUI—Quitovac; SLG—Sierra La Gloria; CAL—Cerro Álamo; CP—Cerro Prieto; SA—Sierra del Álamo; CR—Cerro El Rajón; SSR—Sierra Santa Rosa; BIZ—Bizani; RB—Rancho Bámuri; SL...
Series: GSA Field Guides
Published: 01 January 2017
DOI: 10.1130/2017.0045(02)
EISBN: 9780813756455
... Ana Mountains are located along the Orange and Riverside County boundary in southern California, southeast of Los Angeles, and trend 97 km (~60 mi.) in a NW-SE direction, are 32-km- (20-mi.-) wide, and include ~2226 km 2 (550,000 acres). They form the southern boundary of the Los Angeles Basin...
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Series: Geological Society, London, Special Publications
Published: 01 January 2009
DOI: 10.1144/SP328.2
EISBN: 9781862395763
... and Tireo complexes, overthrusts northeastward above the Loma Caribe–Ortega (LC) unit, which in turn overthrusts the Maimon–Amina and Los Ranchos units, which are separated by the Hatillo Thrust. Southwestward the CC overthrusts the Late Cretaceous–Palaeogene terrigenous sequences of the Trois Rivieres belt...
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Series: AAPG Memoir
Published: 01 January 2003
DOI: 10.1306/M79877C6
EISBN: 9781629810546
... will be deferred until the next section. Stiles et al. (1999) have proposed that all the units in the Villa de Cura Group are of island arc origin. Whereas we accept that the Santa Isabel, El Chino, and El Cano formations are of island arc affinity, i.e., they possess La pmn /Nb pmn ⪢1 ( Figure 4b ), our new...
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