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Vicente Guerrero Formation

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Journal Article

LOWER MISSISSIPPIAN (OSAGEAN) SPIRE-BEARING BRACHIOPODS FROM CAÑÓN DE LA PEREGRINA, NORTH OF CIUDAD VICTORIA, TAMAULIPAS, NORTHEASTERN MÉXICO

FRANCISCO SOUR-TOVAR, FERNANDO ÁLVAREZ, MARÍA LUISA MARTÍNEZ CHACÓN
Published: 01 May 2005
Journal of Paleontology (2005) 79 (3): 469–485.
DOI: https://doi.org/10.1666/0022-3360(2005)079<0469:LMOSBF>2.0.CO;2
...FRANCISCO SOUR-TOVAR; FERNANDO ÁLVAREZ; MARÍA LUISA MARTÍNEZ CHACÓN Abstract Brachiopods are common in the lower and middle parts of the early Mississippian (Osagean) Vicente Guerrero Formation that is mainly a fine-grained quartz arenite found in the Ciudad Victoria area, Tamaulipas...
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Figure 10 — 1–4, Punctospirifer sp., 1, 2, ventral internal ( 1 ) and ...

Published: 01 May 2005
Figure 10 — 1–4, Punctospirifer sp., 1, 2, ventral internal ( 1 ) and external ( 2 ) molds, FCMP/M2-190a-b, from the Lower Member of the Vicente Guerrero Formation at its type locality (FCMP/M2); 3, 4, dorsal internal ( 3 ) and external ( 4 ) molds with some shell still preserved, FCMP/ M2
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Figure 4 — 1–6, Cleiothyridina cf. tenuilineata ( Rowley, 1900 ), all ...

Published: 01 May 2005
Figure 4 — 1–6, Cleiothyridina cf. tenuilineata ( Rowley, 1900 ), all from the Middle Member of the Vicente Guerrero Formation, at its type locality (FCMP/M2). 1, 2, Ventral external ( 1 ) and internal ( 2 ) molds, FCMP/M2-50a-b, ×2.5; 3, detail of umbonal area of ventral internal mold
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Figure 6 — 1–8, Tylothyris ? sp., all from the Middle Member of the Vicen...

Published: 01 May 2005
Figure 6 — 1–8, Tylothyris ? sp., all from the Middle Member of the Vicente Guerrero Formation at its type locality (FCMP/M2) unless otherwise indicated; 1–3, ventral ( 1 ) and posterior ( 2 ) views of a ventral internal mold (FCMP/M2-250b), and dorsal view of a ventral external mold ( 3
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Figure 7 — 1–7, Torynifer pseudolineatus ( Hall, 1858 ), all from the Mi...

Published: 01 May 2005
Figure 7 — 1–7, Torynifer pseudolineatus ( Hall, 1858 ), all from the Middle Member of the Vicente Guerrero Formation at its type locality (FCMP/ M2) unless otherwise indicated; 1, 2, dorsal internal mold, general view ( 1 ) and detail of ctenophoridium ( 2 ), FCMP/M2-220, ×1, ×3, respectively
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Figure 3 — 1–8, Lamellosathyris lamellosa ( Léveillé, 1835 ), all from...

Published: 01 May 2005
Figure 3 — 1–8, Lamellosathyris lamellosa ( Léveillé, 1835 ), all from the Middle Member of the Vicente Guerrero Formation ( Fig. 2 ), at its type locality (FCMP/M2), northeast of Rancho Vicente Guerrero ( Fig. 1 ). 1–4, Ventral internal molds on ventral ( 1, 3 ) and posterior views ( 2, 4
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Figure 2 —Composite stratigraphic section of the Paleozoic and Jurassic st...

Published: 01 May 2005
of the Vicente Guerrero Formation
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Figure 9 — 1–3, Syringothyris ? sp., all from the Lower Member of the Vic...

Published: 01 May 2005
Figure 9 — 1–3, Syringothyris ? sp., all from the Lower Member of the Vicente Guerrero Formation at its type locality (FCMP/M2); 1, three dorsal internal molds with most of dorsal valves still preserved, FCMP/ M2-176 (top), 177 (left), 178 (bottom), ×1; 2, dorsal internal mold with most
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Figure 5 — 1–9, Alispirifer tamaulipensis n. sp., all from the Middle Me...

Published: 01 May 2005
Figure 5 — 1–9, Alispirifer tamaulipensis n. sp., all from the Middle Member of the Vicente Guerrero Formation, at its type locality (FCMP/M2). 1–3, Holotype, ventral ( 1 ) and posterior ( 2 ) views of the ventral internal mold (FCMP/M2-181b), and dorsal view of the ventral external mold ( 3
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Figure 8 — 1–12, Syringothyris cf. typa Winchell, 1863 , all from the ...

Published: 01 May 2005
Figure 8 — 1–12, Syringothyris cf. typa Winchell, 1863 , all from the Middle Member of the Vicente Guerrero Formation at its type locality (FCMP/ M2); 1–3, dorsal, ventral, and anterior views of tectonically deformed internal mold, FCMP/M2-121, ×1; 4–6, dorsal, ventral, and anterior views
Journal Article

Lower Cretaceous Pre-Batholithic Rocks of Northern Baja California, Mexico: GEOLOGICAL NOTES

L. T. Silver, F. G. Stehli, C. R. Allen
Journal: AAPG Bulletin
Published: 01 December 1963
AAPG Bulletin (1963) 47 (12): 2054–2059.
DOI: https://doi.org/10.1306/BC743B99-16BE-11D7-8645000102C1865D
... methods are now being applied to minerals from these same rocks. Following intrusion of the batholithic rocks in Baja California, marine sedimentation resumed in the Ensenada-Colonia Guerrero area in Late Cretaceous time. The post-batholithic Cretaceous rocks are all placed in the Rosario formation...
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The Las Hoyas Lagerstätte: a palaeontological view of an Early Cretaceous wetland

Jesús Marugán-Lobón, Hugo Martín-Abad, Ángela D. Buscalioni
Published: 03 April 2023
Journal of the Geological Society (2023) 180 (3): jgs2022-079.
DOI: https://doi.org/10.1144/jgs2022-079
... and formation of impressions and replicas of vertebrates and invertebrates . Scientific Reports , 6 , 25716 , https://doi.org/10.1038/srep25716 Iniesto , M. , Villalba , I. , Buscalioni , A.D. , Guerrero , M.C. and López-Archilla , A.I. 2017 . The effect of microbial mats...
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Mélanges in southern Mexico: geochemistry and metamorphism of Las Ollas complex (Guerrero terrane)

Oscar Talavera Mendoza
Published: 01 September 2000
Canadian Journal of Earth Sciences (2000) 37 (9): 1309–1320.
DOI: https://doi.org/10.1139/e00-033
... by Delgado et al. ( 1992 ) on brown (magmatic) amphibole from several gabbro dikes intruding LOC at Puerto Vicente Guerrero range from 112 ± 3 to 96.3 ± 2.5 Ma (Albian – lower Cenomanian), which could be considered as the minimum age of the complex. However, the whole-rock Rb–Sr isochron of 311 ± 30 Ma...
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Petroleum Developments in Mexico in 1968

Ricardo Acosta-Estévez
Journal: AAPG Bulletin
Published: 01 August 1969
AAPG Bulletin (1969) 53 (8): 1564–1577.
DOI: https://doi.org/10.1306/5D25C875-16C1-11D7-8645000102C1865D
... as a gas producer in 2 sandstones of the marine Frio Formation (Oligocene). Completion was in the intervals 2,601–2,605 and 2,608–2,612 m. These are new producing reservoirs in this field. The IP was 2,327 Mcf. San Vicente No. 1-A .—This well is 1,600 m N 46° W of Valadeces No. 1...
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Journal Article

Tectonics of México

Manuel Alvarez, Jr.
Journal: AAPG Bulletin
Published: 01 August 1949
AAPG Bulletin (1949) 33 (8): 1319–1335.
DOI: https://doi.org/10.1306/3D933DD0-16B1-11D7-8645000102C1865D
... of Guerrero and Oaxaca, and the small massifs of Guerrero and Michoacan; in addition, the massif of Jalisco and those of Lower California, besides a probable massif in the area southwest of Huimanguillo; finally, the western continent, which comprises the western Sierra Madre and the Mesa Central. Those...
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Sedimentary evolution of a Late Triassic salt giant and a synchronous carbonate unit between the Peruvian Andean Cordillera and the Brazilian Amazonian foreland

Emilio Carrillo, Roberto Barragán, Christian Hurtado, Ysabel Calderón, Germán Martín, Elizabeth Mariño, Luis Sarmiento, Ariana Rivera, Yaniel Misael Vázquez-Taset, Lluís Fontboté, Silvia Rosas
Journal: AAPG Bulletin
Published: 01 January 2023
AAPG Bulletin (2023) 107 (1): 123–150.
DOI: https://doi.org/10.1306/08072221104
... environment interpretations in the SCTZ ( Figures 5 , 11 ), a sedimentary evolution with seven stages is proposed ( Figure 12 ). We interpret unit F in Huallaga–Ucayali as coeval with the Aramachay Formation in San Vicente. Thickening of the studied units, from Yahuish to the Oxapampa and Rio de Moura wells...
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Journal Article

LONGEVITY OF PORPHYRY COPPER FORMATION AT QUELLAVECO, PERU

Richard H. Sillitoe, James K. Mortensen
Journal: Economic Geology
Published: 01 September 2010
Economic Geology (2010) 105 (6): 1157–1162.
DOI: https://doi.org/10.2113/econgeo.105.6.1157
... because it is more difficult, if not impossible, to date the full sequence of events involved in porphyry copper formation. Fig. 1 Location and geology of the Quellaveco porphyry copper-molybdenum deposit, southern Peru. (a) Location map, showing the northern part of the Paleocene to early Eocene...
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Journal Article

Interacting tectonic faulting, karst subsidence, diapirism and continental sedimentation in Pleistocene deposits of the central Ebro Basin (Spain)

JOSÉ LUIS SIMÓN, MARÍA ASUNCIÓN SORIANO, ANTONIO PÉREZ, ARÁNZAZU LUZÓN, ANDRÉS POCOVÍ, HÉCTOR GIL
Published: 14 May 2014
Geological Magazine (2014) 151 (6): 1115–1134.
DOI: https://doi.org/10.1017/S0016756814000156
... structures, reflecting either slow sinking or a sudden collapse of sediments overlying karstified rocks (e.g. Soriano & Simón, 1995 ; Beck, 2004 ; Waltham, Bell & Culshaw, 2005 ; Gutiérrez, Guerrero & Lucha, 2008 ); and (v) ice wedge casts and other structures...
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Mesozoic to Cenozoic deformation of the western Central Andes: an update from structural and U–Pb data of the Calama Basin and surrounding areas

F. Martínez, C. López, A. Patiño, M. Parra, R. González, C. Torres
Published: 31 January 2025
Journal of the Geological Society (2025) 182 (2): jgs2024-055.
DOI: https://doi.org/10.1144/jgs2024-055
... metallic deposits. Today, its tectonic evolution is accepted as being marked by different episodes of extension, contraction and magmatism ( Reutter et al. 1996 ; Tomlinson and Blanco 1997 ; Mpodozis et al. 2005 ; Arriagada et al. 2006 ; Vicente 2006 ; Amilibia et al. 2008 ; Mpodozis...
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Andean topographic growth and basement uplift in southern Colombia: Implications for the evolution of the Magdalena, Orinoco, and Amazon river systems

Veronica J. Anderson, Brian K. Horton, Joel E. Saylor, Andrés Mora, Eliseo Tesón, Daniel O. Breecker, Richard A. Ketcham
Journal: Geosphere
Published: 01 August 2016
Geosphere (2016) 12 (4): 1235–1256.
DOI: https://doi.org/10.1130/GES01294.1
... ). For the upper Miocene Gigante Formation, exposed primarily in the southern Neiva Basin, we use the nomenclature of van der Wiel et al. (1992) , although their Honda divisions differ slightly from those of Guerrero (1997) . Figure 3. Chronostratigraphic framework for the Upper Magdalena Valley (Neiva...
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