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Rio San Pedro Mexico

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Series: GSA Special Papers
Published: 01 April 2013
DOI: 10.1130/2013.2494(04)
... that make up the Rio Grande rift. Rift-sediment thicknesses for the central San Luis Basin determined from a three-dimensional gravity inversion indicate that syn-rift Santa Fe Group sediments have a maximum thickness of ~2 km in the Sanchez graben near the eastern margin of the basin along the central...
Journal Article
Journal: GSA Bulletin
Published: 01 March 2004
GSA Bulletin (2004) 116 (3-4): 259–276.
... America Trench, outline a crustal segment referred to as the Jalisco block ( Luhr and Carmichael, 1981 ). The Ceboruco–San Pedro volcanic field is located in Nayarit, Mexico, northwest of Guadalajara ( Fig. 1 ). It is part of the western Trans-Mexican volcanic belt, a volcanic arc related...
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Journal Article
Published: 14 February 2018
Seismological Research Letters (2018) 89 (2A): 392–398.
... on estimates of current plate motions , Geophys. Res. Lett. 21 , 2191 – 2194 , doi: 10.1029/94GL02118 . Denyer P. Montero W. , and Alvarado G. E. 2003 . Atlas Tectónico de Costa Rica , Editorial Universidad de Costa Rica , San José, Costa Rica (in Spanish). Fan G. Beck...
FIGURES
Journal Article
Journal: AAPG Bulletin
Published: 01 October 2011
AAPG Bulletin (2011) 95 (10): 1667–1698.
...Hugo Matias; Pedro Kress; Pedro Terrinha; Webster Mohriak; Paulo T. L. Menezes; Luis Matias; Fernando Santos; Frode Sandnes Abstract This study presents the results from the interpretation of an extensive and recent regional two-dimensional seismic survey focused on the understanding of the salt...
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Series: AAPG Memoir
Published: 01 January 2013
DOI: 10.1306/13351552M1003532
EISBN: 9781629810010
...) conducted comparative studies in tectonic styles generated by gliding over salt and shale in the Gulf of Mexico and offshore Nigeria, respectively. They concluded that allochthonous structures on a large scale are unique to salt basins, and salt appears to be more mobile in the Gulf of Mexico than...
Journal Article
Journal: Geosphere
Published: 01 October 2010
Geosphere (2010) 6 (5): 621–640.
... for both provinces is illustrated in Figure 2 . By the last revision of the early Mesozoic stratigraphy from the region, Rueda-Gaxiola et al. (1993 , 1999) proposed the Los San Pedros allogroup, which includes a basal volcanogenic unit in the Rio Blanco allomember, which is overlain by a volcano...
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Journal Article
Published: 01 July 2013
Journal of Paleontology (2013) 87 (4): 726–754.
... rudissimus (Trechmann), the hippuritids Caribbea muellerriedi (Vermunt) and Praebarrettia sparcilirata (Whitfield) sensu lato, and the plagioptychids Coralliochama gbohemi Böse and Mitrocaprina tschoppi (Palmer) is described from the Cárdenas Formation in San Luis Potosí State, Mexico. Abundant fossil...
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Journal Article
Published: 01 December 2010
Bulletin of the Seismological Society of America (2010) 100 (6): 3097–3129.
...) and Stewart et al. (1980) . The Limón and Pedro Miguel faults are shown, as are the Rio Gatún and Miraflores faults. Note that there are many small, unnamed faults also mapped in the vicinity of the Canal where exposures allowed for their recognition. The location of the branch of the Camino de Cruces...
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Series: GSA Field Guide
Published: 07 September 2016
DOI: 10.1130/2016.0044(13)
EISBN: 9780813756448
..., formed the Rio Grande gorge, and ultimately, integrated the Rio Grande from Colorado to the Gulf of Mexico. Waning Pleistocene neotectonic activity and onset of major glacial episodes, in particular Marine Isotope Stages 11–2 (~420–14 ka), induced basin fill, spillover, and erosion of the southern San...
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Journal Article
Journal: Geosphere
Published: 01 October 2013
Geosphere (2013) 9 (5): 1161–1200.
...-Pb zircon age ( Duque-Trujillo et al., 2013 ), by the occurrence of Late Paleocene detrital zircons in modern sands from the Acaponeta and San Pedro Rivers, the catchment areas of which include inaccessible areas of the southern SMO ( Fletcher et al., 2007 , their samples SM1 and SM 2), as well...
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Journal Article
Published: 01 August 2001
Clays and Clay Minerals (2001) 49 (4): 318–332.
FIGURES | View All (7)
Journal Article
Journal: GSA Bulletin
Published: 01 April 1953
GSA Bulletin (1953) 64 (4): 459–508.
...CHARLES E STEARNS Abstract The Galisteo-Tonque area lies on the east margin of the Rio Grande Depression, in north-central New Mexico. It extends from the north end of the Sandia Mountains to the south end of the Sangre de Cristo Mountains. The Eocene Galisteo formation, deposited by streams...
Journal Article
Journal: GSA Bulletin
Published: 01 December 1981
GSA Bulletin (1981) 92 (12_Part_II): 2401–2483.
..., and provenance of the Abiquiu Formation, which crops out in Rio Arriba and Sandoval Counties in northern New Mexico (Fig. 1). Many workers have summarized and extrapolated Smith's work (Bingler, 1968; Church and Hack, 1939; Galusha and Bick, 1971; Smith and Muehlberger, 1960; Smith and others, 1970...
Journal Article
Journal: AAPG Bulletin
Published: 01 April 1936
AAPG Bulletin (1936) 20 (4): 467–477.
..., across bridge. 7 hours, 20 minutes). Turn back on same road 160.7 Road fork, take left fork (same as at 160.9) 160.8 Arroyo San Pedro, cross arroyo, then turn left and follow telephone line 170.6 Rancherias. Turn right, leave telephone line 173.3 Rancherias Camp of Ohio-Mexico Oil...
FIGURES
Journal Article
Journal: Palynology
Published: 03 April 2019
Palynology (2019) 43 (2): 188–212.
... occurring in Mexico and Central America ( M. occidentalis ), one widely distributed throughout the neotropics ( M. setosa var. paludosa ), and two in South America ( M. irrigua and M. daleoides ). Mimosa pollen grains are associated in polyads (12 grains), octads and tetrads. Polyads and octads in members...
Journal Article
Published: 01 August 2013
Journal of Sedimentary Research (2013) 83 (8): 562–590.
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Series: GSA Field Guide
Published: 01 January 2012
DOI: 10.1130/2012.0025(08)
EISBN: 9780813756257
... at 09:00 from Hotel Misión, Juriquilla ( Fig. 10 ) and will drive 19 km south toward Querétaro. Turn left into highway 57 to Mexico City for ∼118 km, pass by San Juan del Río and Polotitlán until junction with the Arco Norte highway (route 57D). Turn left and drive for 86 km to junction with route 136...
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Journal Article
Journal: GSA Bulletin
Published: 01 November 2010
GSA Bulletin (2010) 122 (11-12): 1846–1864.
... segment is characterized by dominant dip-slip faulting and therefore is already part of the stress-field domain, where the borehole-breakout data indicate compression perpendicular to the structures. The Rio Gazaunta separates two segments in the region north of the southern tip of the Guaicaramo...
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Journal Article
Journal: AAPG Bulletin
Published: 01 November 1965
AAPG Bulletin (1965) 49 (11): 2041–2075.
... eastern part foundered to form the San Luis basin, which is the northern part of the complex Rio Grande trough. The northwestern part of the San Luis basin merges into the eastern flank of the San Juan Mountains uplift. The southwestern part of the basin is bounded by the east-tilted Brazos uplift...
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Journal Article
Journal: Geosphere
Published: 01 February 2011
Geosphere (2011) 7 (1): 121–144.
... Gulf of Mexico region are less well constrained. For example, the Chiapas massif can be reconstructed in the Río Grande embayment or in the Burgos Basin prior to opening of the Gulf of Mexico. Similarly, the orientation of the continental rift basins that preceded opening of the gulf is uncertain...
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