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Gravity residual anomalies and geothermics in Latium region (Central Italy)
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Autores
Orientador(es)
Resumo(s)
Going from the thyrrenian coast towards the Apennines (SW-NE), a general decrease in Bouguer anomaly values characterizes the Latium gravimetric field. This feature can be referred·to a Moho progressive deepening. A sequence of higher order anomalies is superimposed on this background (first order regional field); these higher order anomalies can be ascribed to thickness variations of a light cover (pyroclastics, shales, sands etc. with a density of 2.00-2.40) overlying a thick, mostly carbonatic basement having a density of 2.60-2.70 and forming the major geothermal reservoir. […].
Descrição
International Symposium on the Activity of Oceanic Volcanoes. Ponta Delgada, 4-9 August 1980.
Palavras-chave
Geothermal Fields Latium Region Italy
Contexto Educativo
Citação
FILIPPO, M.; TORO, B. (1982). Gravity residual anomalies and geothermics in Latium region (Central Italy). "Arquipélago. Série Ciências da Natureza", 3: 269-270.