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The full abstract for this thesis is available in the body of the thesis, and will be available when the embargo expires.
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The Larderello-Travale Geothermal Field in South-West Tuscany (Italy) is the oldest and among the most productive geothermal fields in the world. A new 3D model of seismic P-wave velocity (VP) of the upper crust beneath the geothermal field is derived by inverting a set of highly consistent travel-times from local-earthquakes. Results document a marked correlation of VP with previously described, high-reflectivity horizons. We also determined a low velocity body (VP ∼5 km s−1) culminating at depths of about 7 km, with estimated volume of 35–40 km3. Such low velocities are consistent with a granite at temperatures above 700 °C, thus in a partially-molten status.,Geothermics, 83,
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The full abstract for this thesis is available in the body of the thesis, and will be available when the embargo expires.
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The full abstract for this thesis is available in the body of the thesis, and will be available when the embargo expires.
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The full abstract for this thesis is available in the body of the thesis, and will be available when the embargo expires.
Data Types:
  • Document
The full abstract for this thesis is available in the body of the thesis, and will be available when the embargo expires.
Data Types:
  • Document
Data Types:
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The full abstract for this thesis is available in the body of the thesis, and will be available when the embargo expires.
Data Types:
  • Document
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