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The source of this anomaly was interpreted to be a fluid-enriched lower-crustal region that experienced prograde metamorphism.
This anomaly was interpreted as a widespread partial melting zone and source for free fluids at seismogenic depths.
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Flat spot DHI anomaly is interpreted with possible description of gas water contact areas.
Geological characteristics of the DHI anomalies are interpreted as: 1.
Short wavelength positive magnetic features that correlate with negative gravity anomalies are interpreted to represent shallower granitic intrusions.
Short wavelength magnetic anomalies and co-located low intensity Bouguer gravity anomalies are interpreted to represent shallow and variously magnetized granitic intrusions.
The seismic structural anomalies are interpreted to be aqueous fluid networks located beneath the source region of the swarm that affected the rupture nucleation (e.g., Zhao 2015).
These high-amplitude anomalies are interpreted as bright spots, indicating the presence of oil and gas, as explained by Tanveer (2012).
The shallow (< 200 m) low resistivity anomaly "C1" was interpreted earlier in Amatyakul et al. (2016) as a manifestation of the hot springs.
Finally, similar to FCC, the anomaly of elements was interpreted based on the composition of the obtained colors.
Okada et al. (2010) indicated a low-velocity (Vs) anomaly in this area that was interpreted as partial melting.
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