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The preferred 3D resistivity models show that a moderately resistive structure (30 200 Ω m) is characteristic of most of the volcano, and were able to delineate a hydrothermal zone within the volcanic edifice.
At an elevation of 2000 m, the entire area is dominated by a uniform moderately resistive structure (40 200 Ω m) with embedded high-resistivity blocks (>800 Ω m).
The interpreted resistivity model under the Main Pyramid displayed a highly resistive structure towards its northern face that could be associated with infill.
This resistive structure implies an asperity zone of the NAF, which was ruptured in 1943.
At the high elevation of 2700 m, a moderately resistive structure (50 320 Ω m) dominates the whole area.
A highly resistive structure cuts through the conductors between sites ram and yan (see Figure4a, (B) and Additional file1).
Similar(50)
For example, MT studies (Wannamaker and Doerner, 2002) conducted in the Ruby mountains imaged resistive structures close to deep crustal, steeply dipping fault zones.
The Marine Controlled-Source ElectroMCSEMtic (method methas has been recognized as an important and effective tool to detect electrically resistive structures, such as oil, gas, and gas hydrate.
The resistive structures are located on a suspended, thereby, thermally isolating, low mechanical stress membrane and integrated into a glass flow channel.
Figure 8 shows the resistivity model derived from 2-D inversion of the MT data together with major identified surface geological features, in order to understand the relationship between tectonic and geological processes and the resistive structures.
Resistive structures on both sides of the fault beneath this transition suggest that the lack of seismicity might be related to the absence of fluid pathways in the seismogenic zone.
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