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dc.contributor.advisorEverett, Mark
dc.creatorAmara, Akhil
dc.date.accessioned2016-09-22T19:46:48Z
dc.date.available2016-09-22T19:46:48Z
dc.date.created2016-08
dc.date.issued2016-07-01
dc.date.submittedAugust 2016
dc.identifier.urihttp://hdl.handle.net/1969.1/158038
dc.description.abstractA multi-azimuth and multi-polarization ground penetrating radar (GPR) survey is carried out to help characterize a fractured fault zone located in Mason County, Texas. A total of 36 lines were acquired on and near the fault zone to try to identify the GPR signature of a complex fracture system. These lines were run through a standard set of processing steps to try to identify the fractures. The results showed that the multi-azimuth survey helped identify the dominant strike of the fractures, which was parallel to the strike of the fault (NE-SW). The multi-polarization survey helped identify the different fills of the fractures. Due to the orientation of the fractures, the PP orientation showed the resistive fractures while the TT orientation showed the conductive fractures. gprMax, a 2-D finite-difference time-domain GPR simulation software, was used to confirm the results seen in the field data. Two 2-D models were created to understand the GPR response of the different fracture fills in the TT orientation. The first model simulated 3 identical fractures with 3 different fracture fills (air, water, clay). Results of this model showed that in the TT orientation, the air filled fractures have the weakest response while the clay filled fractures have the strongest response. The second model simulated the dominant fractures seen in Line A, PP and TT orientations. The results again showed that in the TT orientation, conductive fractures have the strongest response while the resistive fractures have the weakest response, confirming the results from the field data. A geophysical workflow was proposed to help identify buried shallow faults in remote locations. This workflow will help enhance the field observations of an area. The workflow goes from surveying a large area (100s of m) using aeromagnetic data to identifying fractures in a fault zone at cm scale by using GPR method shown in this research.
dc.format.mimetypeapplication/pdf
dc.language.isoen
dc.subjectGPR
dc.subjectfault
dc.subjectfault zone
dc.subjectfractures
dc.subjectMulti-Azimuth
dc.subjectMulti-Polarization
dc.subjectgeophysical workflow
dc.titleUsing Multi-Azimuth and Multi-Polarization Ground Penetrating Radar to Characterize a Fractured Fault Zone in Mason County, Texas
dc.typeThesis
thesis.degree.departmentGeology and Geophysics
thesis.degree.disciplineGeophysics
thesis.degree.grantorTexas A & M University
thesis.degree.nameMaster of Science
thesis.degree.levelMasters
dc.contributor.committeeMemberReece, Bobby
dc.contributor.committeeMemberHouser, Chris
dc.type.materialtext
dc.date.updated2016-09-22T19:46:48Z
local.etdauthor.orcid0000-0003-2003-4825


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