Abstract
We present a new method for interpretation of potential-field anomaly data. A linear equation, involving the anomaly and its horizontal gradient, is derived to provide both the depth and nature of the buried sources. The proposed method is similar to the Euler technique; however, it uses a shape factor (q) instead of a structural index (η) to characterize the buried sources. The method is tested using theoretical simulations with different gravity and magnetic models placed at different depths with respect to the observation height. In all cases, the method adequately estimated the locations and the approximate shapes of the sources. Results from field examples will be discussed at the meeting.
Original language | English |
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State | Published - 2002 |
Event | 2002 Society of Exploration Geophysicists Annual Meeting, SEG 2002 - Salt Lake City, United States Duration: Oct 6 2002 → Oct 11 2002 |
Conference
Conference | 2002 Society of Exploration Geophysicists Annual Meeting, SEG 2002 |
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Country/Territory | United States |
City | Salt Lake City |
Period | 10/6/02 → 10/11/02 |
Bibliographical note
Publisher Copyright:© 2002 SEG Annual Meeting. All Rights Reserved.
ASJC Scopus subject areas
- Geophysics