| 2007 GSA Denver Annual Meeting (28–31 October 2007) | |
| Paper No. 209-30 | |
| Presentation Time: 8:00 AM-12:00 PM | ||
REMOTE DETECTION AND GEOCHEMICAL STUDIES FOR FINDING HYDROCARBON-INDUCED ALTERATIONS IN LISBON VALLEY, UTAH, AND GARZA FIELD, TEXAS | ||
|
PETROVIC, Ana, Geosciences, University of Houston, 4800 Calhoun Rd, 312 S&R1, Houston, TX 77204-5507, apetrov2@mail.uh.edu and KHAN, Shuhab D., Geosciences, University of Houston, 4800 Calhoun Rd. 312 S&R1, Houston, TX 77204-5507 Long-term leakages of hydrocarbons develop diverse array of chemical and mineralogical changes in the form of alterations of rocks and soils. Alterations caused by microseepages are reported to have affected sandstones of Wingate Formation in Lisbon Valley, Utah, and of Dockum Group in Garza field, Texas. Alterations in Lisbon Valley include bleaching of redbeds, anomalous limonite and carbonate concentrations, anomalous weathering patterns and anomalous clay content. This study has developed new methodologies using spectroscopy, HYPERION hyperspectral and ASTER multispectral remote sensing data, Synthetic Aperture Radar data, and geochemical analyses (thin sections, ICP-AES analyses, carbon isotopes) to identify and map these changes and confirm the hydrocarbon microseepages source in Lisbon Valley. Using ASTER and HYPERION satellite images and SAR data, the altered areas of the Wingate Formation were identified and mapped at the northwest and southwest part of the Lisbon Valley anticline. Based on alterations three different zones were identified in the Wingate Formation; the southwest zone is the most altered, the middle part is unaltered, and the northwest part shows minor alterations. Spectroscopy and thin section studies revealed higher content of clay minerals in altered than in unaltered zones. Major elemental concentrations suggest removal of iron cement and addition of calcite during diagenesis. Trace elemental concentrations in selected altered sandstone samples are characteristic of geochemical halos forming over oil fields. Currently we are applying similar techniques in Garza field, Texas. Garza field is located along the northeast edge of the Permian basin. Producing rocks have an average depth of around 800m, and are overlain by red shales and sandstones of Dockum Group. Sandstones are in some areas discolored and those bleached mounds are then distributed in narrow areas. Bleaching of redbeds has previously been reported in Garza oil field, Texas, but no detailed work regarding analyses of hydrocarbon-induced alterations has been done. This methodology provides a new technique for petroleum exploration for use in remote regions of the world where the field work is difficult. | ||
|
2007 GSA Denver Annual Meeting (28–31 October 2007)
General Information for this Meeting | ||
| Session No. 209--Booth# 150 Planetary Geology: Potpourri (Posters) Colorado Convention Center: Exhibit Hall E/F 8:00 AM-12:00 PM, Wednesday, 31 October 2007 Geological Society of America Abstracts with Programs, Vol. 39, No. 6, p. 572 | ||
© Copyright 2007 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. | ||