1887

Abstract

The Larderello geothermal reservoir is locally situated in Paleozoic phyllites and quartzites. Permeability is controlled by fractures. The reservoir is identified with a fractured zone usually not more than 150 meters thick and located at the top of the Paleozoic basement.

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/content/papers/10.3997/2214-4609.201410811
1991-05-28
2020-09-25
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