The relationship between extensional brittle shear zones and deep-seated granitoids is investigated by means of reflection seismic lines in the Larderello geothermal field. The interpretation of these lines was based on field data and borehole stratigraphies. A deep-seated granitoid and three main and parallel extensional brittle shear zones, north-eastward dipping, were recognised in the crust of the Larderello zone. The capacity of reflection seismic to define possible hydrological pathways in geothermal areas is underlined by the results of this study.
Scheda prodotto non validato
Attenzione! I dati visualizzati non sono stati sottoposti a validazione da parte dell'ateneo
|Titolo:||Extensional brittle shear zones and deep seated granitoid in the Larderello field|
|Data di pubblicazione:||2002|
|Appare nelle tipologie:||4.2 Abstract in Atti di convegno|