Quick
Search: 
 
advanced search
 GSW Home    GeoRef Home    My GSW Alerts    Contact GSW    About GSW    Journals List    Help 
Journal of Environmental & Engineering Geophysics Signup for GSW Email News
JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS

Journal of Environmental & Engineering Geophysics; June 2007; v. 12; issue. p. 149-161; DOI: 10.2113/JEEG12.2.149
© 2007 Environmental & Engineering Geophysical Society
This Article
Right arrow Figures Only
Right arrow Full Text
Right arrow Full Text (PDF)
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Similar articles in Web of Science
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Citing Articles
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Khatun, S.
Right arrow Articles by Keller, G.R.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Research Articles

Locating Faults in the Southern Mesilla Bolson, West Texas and Southern New Mexico, Using 3-D Modeling of Precision Gravity Data

S. Khatun, D.I. Doser, E.C. Imana and G.R. Keller

Department of Geological Sciences, University of Texas at El Paso El Paso, TX 79968

In this study, we have used precision gravity surveys to investigate the subsurface structure of groundwater basins in the El Paso, Texas region. This study focused on finding smaller faults within the Mesilla bolson (basin), which are believed to be a major control on ground water flow. The Mesilla bolson serves as one of two major aquifers for the city/county of El Paso. A previous 2-D gravity modeling study of data collected along three east-west trending lines had suggested that the eastern boundary of the Mesilla bolson is controlled by a series of smaller faults, rather than a single large one. Our study uses 3-D modeling techniques to more accurately locate these faults. Additional gravity data were also collected along three north-south trending lines. In our gravity modeling approach, topography and near surface geology were included in the model to better determine the detailed structure lying below the surface. The results of this study show that the locations of some of the previously identified faults that likely control groundwater recharge from the surrounding mountains as well as the flow of saline water in the southernmost bolson need to be modified.







JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2009 by Environmental & Engineering Geophysical Society