We utilize a magnetotelluric profile in the Travale geothermal field, in Tuscany,
Italy, to obtain a resistivity model using 2-D inversion of the series and parallel
(S-P) invariant impedances. The idea is to experiment the performance of the S-
P responses as compared with 2-D inversion of conventional TE and TM
impedances. Resembling TE and TM responses, S-P are complementary, as
series impedance is more sensible to galvanic effects while parallel is to
inductive effects. Moreover, as both responses are rotation invariants, they
overcome the trouble of selecting a rotation angle or using a tensor
decomposition technique. For S-P inversion we used a Gauss-Newton algorithm
designed to minimize the data misfit at the same time as the model is kept as
smooth as possible. The trade-off between data misfit and model roughness is
balanced by a regularization factor. We change this factor in a search for the
model with the best tradeoff between data misfit and model roughness. TE and
TM impedances were inverted using the algorithm of Rodi and Mackie, after
rotation of data toward the main strike direction of the area. The resulting TE-
TM and S-P model shows many similarities in defining resistivity anomalies at
both shallow (500 m) and deep (1-5 km) depth. The 2D models show resistivity
anomalies that correlate with zones of high permeability and fluid content
representing exploited geothermal reservoirs. The shallow resistivity anomalies
show a good correlation with the shallow geothermal reservoir, located in
carbonate units. The anomalies are particularly visible in correspondence of the
faults, suggesting an increase of permeability, a pathway for fluids and possible
related alteration minerals. The most conspicuous feature of the 2D models is
the presence of low resistivity anomalies inside the resistive basement at a
depth of 1-4 km b.g.l. This deep resistivity anomaly corresponds to the deep
fractured and highly productive geothermal reservoir located in the
metamorphic rocks. This deep reservoir is made of sparse fractures and hosts
superheated steam.
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