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Post-paleozoic tectonics of northeast mexico and its role in the evolution of the gulf of mexico

R. J. Padilla, +1 more
- 01 Jan 1986 - 
- Vol. 25, Iss: 1, pp 157-206
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TLDR
In this article, a modelo alternativo for the deformación del Terciario Temprano del noreste de Mexico, asi como una serie de paleorreconstrucciones de tectonica de placas, basados principalmente en la existencia of varias fallas sinistrales de transcurrencia, orientadas al noroeste and una falla dextral transcurrente (Falla Tamaulipas-Oaxaca) orientada al nor-noro
Abstract
Se muestra la evolucion sedimentaria mesozoica del noreste de Mexico a traves de varios mapas paleogeograficos regionales. Tambien, con base en diferentes estilos de plegamiento, se propone un modelo alternativo para la deformacion del Terciario Temprano del noreste de Mexico, asi como una serie de paleorreconstrucciones de tectonica de placas, basados principalmente en la existencia de varias fallas sinistrales de transcurrencia, orientadas al noroeste y una falla dextral transcurrente (Falla Tamaulipas-Oaxaca) orientada al nor-noroeste, a lo largo de la cual el bloque de Yucatan se movio hacia el Sur (Jurasico Tardio) desde su antigua position en el sitio que hoy ocupa el Golfo de Mexico.

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Journal ArticleDOI

Paleogeographic Evolution of Early Deep-Water Gulf of Mexico and Margins, Jurassic to Middle Cretaceous (Comanchean)

TL;DR: In this paper, the early Gulf of Mexico is inferred from Cretaceous carbonate shelf margins interpreted from seismic profiles and other stratigraphic data, and hindcasting of subsidence history in the central basin.
Journal ArticleDOI

Evolución geológica del sureste mexicano desde el Mesozoico al presente en el contexto regional del Golfo de México

TL;DR: The geologic evolution of southeastern Mexico is analyzed in the regional context of the Gulf of Mexico, which starts it opening with the fragmentation and spreading of Pangea as discussed by the authors, and the sedimentary record in this depression begins with the deposit of continental red beds during the Late Triassic and Early Jurassic, after which, during the Callovian, sea-waters from the Pacifi c invaded an extense area; low circulation and high evaporation of these waters allowed the deposition of large volumes of salt in the central part of the basin.
Journal ArticleDOI

Tectonic setting and sandstone petrofacies of the Bisbee basin(USA–Mexico)

TL;DR: The Bisbee basin is part of the border rift system as discussed by the authors, which was formed by an eruption of a bimodal mid-Jurassic volcanic assemblage succeeding Early to Middle Jurassic arc volcanism.
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El terreno Cuicateco: ¿cuenca oceánica con influencia de subducción del Cretácico Superior en el sur de México? Nuevos datos estructurales, geoquímicos y geocronológicos

TL;DR: In this paper, Romero et al. present a porcion suroriental del terreno Cuicateco, entre Matias Romero and Juchitan, Oaxaca, which is characterized by a secuencia vulcanosedimentaria of bajo grado metamorfi co that presenta por lo menos¯¯¯¯tres eventos de deformacion, D1: plegamiento recumbente a isoclinal F1 de the superfi cie de estratifi cacion.
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