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Using integrated geophysics data set to delineate Phetchabun active fault in Thailand
Rungroj Arjwech1, Wanwisa Boonsungnern1, Pakawat Sriwangpon1
1Department of Geotechnology, Faculty of Technology, Khon Kaen University, Khon Kaen, 40002, Thailand.
This study precisely located active faults in the Phetchabun basin using remote sensing, gravity surveys, and electrical resistivity tomography. These integrated geophysical methods successfully identified subsurface fault structures, aiding paleo-earthquake investigations.
Area of Science:
- Geophysics
- Structural Geology
- Remote Sensing
Background:
- Precisely locating active faults is crucial for understanding seismic hazards.
- The Phetchabun basin requires detailed geological and geophysical investigation to identify active fault systems.
Purpose of the Study:
- To precisely locate active faults within the Phetchabun basin.
- To integrate multiple geophysical methods for enhanced fault detection and characterization.
Main Methods:
- Remote sensing and Digital Elevation Model (DEM) analysis to identify potential fault traces.
- Geomorphological and geological field investigations to validate remote sensing data.
- Gravity surveys and 2D-3D Electrical Resistivity Tomography (ERT) for subsurface structural analysis.
Main Results:
- Gravity models revealed subsurface density contrasts indicative of vertical fault planes.
- ERT inversion images identified fault planes through zones of varying resistivity.
- The integration of three geophysical surveys provided comprehensive data on active fault locations.
Conclusions:
- The combined geophysical approach effectively delineates active faults in the Phetchabun basin.
- Identified fault structures have significant implications for paleo-earthquake research in the region.
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