Title:

An Interference Test in Alfina Geothermal Field (Northern Latium, Italy)

Authors:

Antonio Barelli and Graziano Manetti

Geo Location:

Alfina, Italy

Conference:

Stanford Geothermal Workshop

Year:

1975

Session:

Well Testing

Language:

English

File Size:

167KB

View File:

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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