This study investigated the usefulness of gravity data in deducinginformation about thenear-surface geological structures which may be controlling geothermalactivity on the island of Vulcano.Gravity measurements were carried out along several profiles takenacross and around the Fossa crater. Aobtained for a simple two layer model including a dense rectangularprism. The dense material beneaththe crater may be the self-sealed volcanics under which geothermalfluids circulate, as inferred by othergeophysical studies.
CITATION STYLE
Sugihara, M., Okuma, S., Nagao, K., Furukawa, R., Komazawa, M., & Supper, R. (2002). Relationship between geothermal activity and gravity anomalies on Vulcano Island, Italy. 24th NZ Geothermal Workshop, 5. Retrieved from http://staff.aist.go.jp/m.sugihara/Vulcang1.pdf
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