Zobrazeno 1 - 10
of 42
pro vyhledávání: '"Gabriel Chávez Cabello"'
Autor:
María I. Hernández-Ocaña, Felipe Torres de la Cruz, Elizabeth Chacón Baca, Samuel Eguiluz de Antuñano, Gabriel Chávez-Cabello
Publikováno v:
Geological Society, London, Special Publications. 522:97-116
An ichnological analysis of the Paleocene–Eocene Wilcox Formation at San José de la Laja and La Curva localities within the Burgos Basin in northeastern Mexico revealed seven ichnogenera: Chondrites , Diplocraterion , Ophiomorpha , Palaeophycus ,
Autor:
Rafael Guerra Roel, Daniel Pastor Galán, Gabriel Chávez Cabello, César Francisco Ramírez-Peña, José Jorge Aranda Gómez, Gerardo Patiño Méndez, Alejandro Rodríguez-Parra, Eduer Giovanny Nova Rodríguez, Roberto Stanley Molina Garza
The Mexican Fold-and-Trust Belt is a winding belt that formed after a series of protracted tectonic events, which began with the onset of sedimentation in the basins formed during the break-up of Pangea and during the roll-back of the oceanic Kula pl
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e387f55f25a8bacc7640f8dfe4abaeaf
https://doi.org/10.5194/egusphere-egu23-324
https://doi.org/10.5194/egusphere-egu23-324
Publikováno v:
Geological Society, London, Special Publications. 504:183-202
Autor:
Elizabeth Chacón-Baca, Felipe Torres de la Cruz, Gabriel Chávez-Cabello, María Isabel Hernández-Ocaña
Publikováno v:
Revista Mexicana de Ciencias Geológicas. 37:9-25
Depositional episodes are readily identified along representative localities of the Lower Cretaceous Cupido platform in northeastern Mexico. The basal part of the Cupido Formation exhibits a progradational reef platform that, at the upper limit, is t
Autor:
César Francisco Ramírez-Peña, Gabriel Chávez-Cabello, Rogelio Sosa Valdés, José Jorge Aranda-Gómez, Elisa Fitz-Díaz
Publikováno v:
Journal of South American Earth Sciences. 93:242-252
In this paper we report U Pb zircon ages from a syn-tectonic magmatism related to a contractional thick-skinned deformation pulse in the Mexican Fold and Thrust Belt. The study area corresponds to the Concepcion del Oro Block (COB), which is located
Autor:
Yam Zul Ernesto Ocampo-Díaz, Gabriel Chávez-Cabello, Ariel Ramírez-Díaz, Jorge Aceves de Alba, Marisol Polet Pinzon-Sotelo, Martín Guerrero-Suastegui
Publikováno v:
Revista Mexicana de Ciencias Geológicas. 36:207-228
Un análisis sedimentológico e icnológico realizado en los miembros Tierras Blancas y Rancho Viejo de la Formación Concepción del Oro (Turoniano-Campaniano temprano), en la región de Concepción del Oro, Zacatecas, permite documentar las caracte
Autor:
María Isabel Hernández-Ocaña, Samuel Eguiluz de Antuñano, Felipe Torres de la Cruz, Gabriel Chávez-Cabello, Elizabeth Chacón-Baca, Sara A. Quiroz-Barroso
Publikováno v:
Journal of South American Earth Sciences. 90:107-117
The present paper address the occurrence of Venericardia shell concentrations distributed over hundreds of meters along terrigenous horizons as a typical sedimentary facies of the Wilcox Formation in the Burgos Basin. These extensive deposits overlie
Publikováno v:
Earth-Science Reviews. 183:56-84
The Mexican orogen is the expression in Mexico of the Cordilleran orogenic system. The orogen extends the length of Mexico, a distance of 2000 km from the state of Sonora in the northwest to the state of Oaxaca in the south. The Mexican orogen consis
Publikováno v:
Journal of Structural Geology. 109:127-139
The Mexican fold-thrust belt in central Mexico excellently exposes relatively well preserved syntectonic deposits that overlay rocks with lateral lithostratigraphic changes across the belt. We consider the deformational effects of these changes by in
Autor:
César Francisco Ramírez-Peña, Sóstenes Méndez-Delgado, Gabriel Chávez-Cabello, Xavier J. Pérez-Aguirre, Oscar Mario Romero-de la Cruz
Publikováno v:
Journal of South American Earth Sciences. 110:103288
On the boundaries of the states of Coahuila and Zacatecas in northern Mexico, scarce outcrops of a Triassic subduction complex have been used to infer in several positions a tectonostratigraphic terranes boundary. This crustal boundary is covered by