Oligocene alkaline igneous activity in NE Mexico-Reference-Cited by-同舟云学术

Oligocene alkaline igneous activity in NE Mexico

Published:1973-11 Issue:6 Volume:110 Page:551-555
ISSN:0016-7568
Container-title:Geological Magazine
language:en
Short-container-title:Geol. Mag.

Author:

Bloomfield K.,Cepeda-Davila L.

Abstract

SummaryPotassium-argon age determinations on rocks from the Sierra de San Carlos, State of Tamaulipas, México, which are petrographically very similar to other bodies in north-eastern México and the south-central U.S.A., indicate that a NW-trending zone of alkaline complexes, at least 1,400 km in length, stretches from the Gulf coast to southern New Mexico. This zone may be structurally related to the parallel, but somewhat younger, Rio Grande rift.

Publisher

Cambridge University Press (CUP)

Subject

Geology

Reference18 articles.

1. Anderson J. E. 1968. Igneous geology of the Central Davis Mountains, Jeff Davis County, Texas. Explanation of Geologic Quadrangle Map No. 36. Bur. Econ. Geol., Univ. Texas.

2. Chapin C. E. 1971. The Rio Grande rift, pt. 1: Modifications and alterations, pp. 191–201. In Guidebook of the San Luis basin, Colorado. New Mexico geol. Soc., 22nd Field Conf.

3. Cenozoic Chronostratigraphy, Planktonic Foraminiferal Zonation and the Radiometric Time Scale

4. Aligned intrusive complexes in northern Coahuila, México (abstract);Daugherty;Spec. Pap. geol. Soc. Am.,1965

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