| 2004 Denver Annual Meeting (November 7–10, 2004) | |
| Paper No. 67-2 | |
| Presentation Time: 8:15 AM-8:30 AM | ||
PROCESSING AND INTERPRETATION OF HIGH-RESOLUTION SEISMIC DATA OF SEDIMENTS WITHIN TICONA CHANNEL, ILLINOIS | ||
|
OJEDA, Anastasiya Andreyevna, Hydrogeology, Illinois State Univ, 606 1/2 Oglesby Ave, #B, Normal, IL 61761, aaojeda@ilstu.edu. High-resolution S-wave seismic profiling was used to improve the resolution of mapping of the quaternary sediments within the Ticona Channel, Illinois. Seismic data was acquired using a 12-channel land-streamer with an array, of two opposite directed 14 Hz geophones per channel, mounted on metal sleds. A 1 kg sledge hammer striking a steel-capped wooden plate weighted by a truck was used to generate horizontal energy. Three profiles 1.5 – 2 miles each of S-wave data was acquired across the Ticona Channel. Data was processed using WinSeis Turbo (KGS) and software of Dr. Andre Pugin(ISGS). Raw data was merged, sorted, filtered and stacked; after velocity analysis NMO correction was applied. Output file was converted to SEG-Y format and imported into Kingdom Suite+ software. This software was used to create cultural map, download topographical map and navigate the seismic survey. We picked horizons and converted time horizons to depth. Contouring the depth map was the last applied function. The results will be use to determine the potential and characteristics of the studied sediments as an aquifer. S-wave profiling allowed us to subdivide quaternary sediments within the Ticona Channel and used to improve resolution of the geological mapping. | ||
|
2004 Denver Annual Meeting (November 7–10, 2004)
General Information for this Meeting | ||
| Session No. 67--Booth# 0 Geophysics/Tectonophysics/Seismology: From Groundwater to North American Tectonics Colorado Convention Center: 102 8:00 AM-12:00 PM, Monday, November 8, 2004 Geological Society of America Abstracts with Programs, Vol. 36, No. 5, p. 172 | ||
© Copyright 2004 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. | ||