9 From Grenvillian Basement to Neotectonics in Northeast Mexico: A 1.3-Billion-Year Journey of Geological Development
Monday, 14 March 2022
1:30 PM - 5:30 PM
Online
CIUDAD VICTORIA BLOCK: PRACAMBRIAN AND PALEOZOIC PERI-GONDWANAN CRUSTAL ASSEMBLAGE FROM NE MEXICO
Paper number: 9-1
Program: Theme Sessions
Time: 1:30 PM – 1:50 PM
Authors
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Eduardo Alejandro Alemán GallardoUniversidad Autonoma de Nuevo Leon, Linares, NL
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Juan Moisés Casas PeñaUniversidad Autónoma de Nuevo León, Linares, NL
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Bodo WeberCenter for Scientific Research and Higher Education of Ensenada, Ensenada, BJ
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Uwe JenchenUniversidad Autónoma de Nuevo León, Linares, NL
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Fernando Velasco TapiaUniversidad Autónoma de Nuevo León, Linares, NL
Abstract
There are several regional crustal blocks scattered in Mexico, developed on the northwester margin of Gondwana near the collision zone with Laurencia, during the closure of the Rheic Ocean and the Pangea amalgamation. Through the dismemberment of this supercontinent and along with the south-wards migration of the Maya Block and the opening of the Gulf of Mexico during the Jurassic, these blocks were dismembered and drifted forming a discontinuous belt, later buried by Mesozoic and Cenozoic sedimentary and volcanic rocks.
This would imply that the basement, Mexico´s geological backbone, is highly segmented and that it is necessary to review the distribution of the vestiges of the Ouachita-Marathon-Sonora orogen. This since evidence of the late Paleozoic collision has been described in localities now situated in southern Mexico. Additionally, it is proposed to abandon the “Sierra Madre Terrane” concept for the SMO basement and instead use that of the “Ciudad Victoria Block”, to include all its different units.
Geological Society of America Abstracts with Programs. Vol. 54, No. 1
doi: 10.1130/abs/2022SC-373875
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