An Interference Test in Alfina Geothermal Field (Northern Latium, Italy)
- Location
- Alfina, Italy
- Conference
- Stanford Geothermal Workshop
- Year
- 1975
- Session
- Well Testing
- Language
- English
Full text
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Abstract
A fina field is situated in central Italy near the Lake of Bolsena. Its geogical- stratigraphical sequence is as follows:
a. A thick (>500 m) Cretaceous-Eocene sedimentary series facies comprising mainly clays and marls. the cap rock; This flysch BOI sena. 1 n flysch series forms
b. A Mesozoic sedimentary series, stratigraphically quite regular, of more than 400 m thickness, comprising mainly carbonates (limestones, marly limestones and calcarenites). This series forms the geothermal aquifer, having a high permeability as a result of the presence of fractured zones.
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