T79 Undergraduate Research Posters Showcasing Research by 2YC and 4YCU Geoscience Students (Posters)

Sunday, 22 October 2017
9:00 AM - 5:30 PM
Halls 4EF


INVESTIGATING POST EMPLACEMENT COOLING HISTORIES AND TECTONIC CAUSE OF EXHUMATION OF IGNOUS INTRUSTIONS IN EL PASO, TX USING APATITE (U-TH)/HE DATA

Paper number: T79-21
Program: Technical Sessions
Time: 9:00 AM – 5:30 PM


Authors


Abstract

The El Paso region of westernmost Texas has experienced multiple episodes of Cenozoic tectonic uplift and erosion. Within this area, several relatively small andesitic intrusive bodies crop out including: the Campus Andesite, Coronado Hills, Cristo Rey, and Three Sisters. Based on geochemical and geophysical studies, the intrusive rocks are genetically related and thought to be the exposed portions of a larger body that underlies much of western El Paso and northern Ciudad Juárez area. Where exposed, this body intrudes into Cretaceous strata, and a two published K-Ar dates suggests that it was intruded 47.1 ± 2.3 Ma, during the waning stages of the Laramide Orogeny. Although previous research has focused on the mineralogy and petrology of this unit, no work has been done to constrain the exhumational history of these intrusions. In order to investigate their post-emplacement history, four samples were collected for apatite (U-Th)/He (AHe) analyses from the Campus Andesite, Coronado Hills, Cristo Rey, and Three Sisters. Five single-grain AHe ages per sample are being obtained. The data will be modeled using HeFTy software in order to provide approximate times of exhumation for each intrusion. The results will be compared to existing AHe ages from the nearby Franklin Mountains to determine if the exhumation and erosion of the intrusive bodies were temporally related to the Laramide Orogeny, or to deformation related to the development of the Rio Grande rift.

Geological Society of America Abstracts with Programs. Vol. 49, No. 6

doi: 10.1130/abs/2017AM-304880

© Copyright 2017 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions.