SEG Technical Program Expanded Abstracts 2014 2014
DOI: 10.1190/segam2014-0964.1
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Structural geology observations derived from full tensor gravity gradiometry over rift systems

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“…Then at least 10 FTG observation points on a profile at right angles to the fault and in close proximity are used to create a characteristic curve using a least squares best fit. Once the closed Txx-Txz curve is established, the dip, throw and density contrast are directly calculated (FitzGerald and Holstein, 2014). Initial applications indicate 3D faults that are sheet-like, can be derived in mining and oil exploration settings that have had a strong tectonic or rift-like history.…”
Section: Faultsmentioning
confidence: 99%
“…Then at least 10 FTG observation points on a profile at right angles to the fault and in close proximity are used to create a characteristic curve using a least squares best fit. Once the closed Txx-Txz curve is established, the dip, throw and density contrast are directly calculated (FitzGerald and Holstein, 2014). Initial applications indicate 3D faults that are sheet-like, can be derived in mining and oil exploration settings that have had a strong tectonic or rift-like history.…”
Section: Faultsmentioning
confidence: 99%