|Northeastern Section (39th Annual) and Southeastern Section (53rd Annual) Joint Meeting (March 25–27, 2004)|
|Paper No. 41-5|
|Presentation Time: 8:00 AM-12:00 PM|
ASSESSING REGIONAL SUBSURFACE VARIABILITY IN THE ATLANTIC COASTAL PLAIN
JONES, Stephanie Brevard, Geological Sciences, Clemson Univ, 340 Brackett Hall, Clemson, SC 29634-0919, email@example.com.|
Traditional methods of assessing the regional subsurface variability of geological parameters are often qualitatively based, and boundaries between regions are subjectively placed without regard for spatial variability or the rate at which the parameters change. Traditional methods also do not allow for comparing the rate of change of one variable with that of another. To minimize the drawbacks of these traditional approaches, a new method was developed for use with geophysical log data. This new method involves characterizing each geophysical log with a high order polynomial expression, which is divided into segments based on the depth at which the polynomial’s first derivatives occur. For those segments whose boundaries (i.e. first derivatives) are identifiable in all wells and are assumed with confidence to be correlative, the polynomial for that segment is expressed by an equal number of uniformly spaced points in every well, regardless of the stratigraphic thickness of the segment. All correlative segments are averaged to establish an “ideal” segment, and the coefficient of determination (R2) is calculated in order to obtain a quantitative measure of the similarity between the “ideal” segments and the correlative segments in a given well. The coefficients of determination for all wells included in the study are mapped and contoured, and the degree of similarity between two well logs is reflected by their location relative to the contours. In addition, orientation of the contours in relation to the strike and dip of the units provides information for interpreting depositional environments and/or diagenesis.
This method for assessing the regional variability of geophysical logs has been applied to select areas of the Atlantic Coastal Plain in South Carolina. A pilot study using numerous closely-spaced wells has been completed, and a larger scale study of the Upper Cretaceous Series throughout the state is underway.
Northeastern Section (39th Annual) and Southeastern Section (53rd Annual) Joint Meeting (March 25–27, 2004)
General Information for this Meeting
|Session No. 41--Booth# 19|
Sedimentation and Stratigraphy II (Posters)
Hilton McLean Tysons Corner: Ballrooms A and B
8:00 AM-12:00 PM, Friday, March 26, 2004
Geological Society of America Abstracts with Programs, Vol. 36, No. 2, p. 90
© 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.