Fig. 4: Relationship between seismicity distribution and resistivity anomaly. | Communications Earth & Environment

Fig. 4: Relationship between seismicity distribution and resistivity anomaly.

From: 3D magnetotelluric imaging of a transcrustal magma system beneath the Campi Flegrei caldera, southern Italy

Fig. 4

The (a) shows the map of the CF area, with elevation represented by a color scale and epicentres of earthquakes (Md > 2.5, since January 2019; white dots). The black lines indicate the α and β profiles used to extract the 3D resistivity sections. b, c display the resistivity cross-sections along α and β profiles, with hypocentress of earthquakes superimposed (white dots). All visualizations of the 3D resistivity models presented in this manuscript were produced using the ParaView software package.

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