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Gravity residual anomalies and geothermics in Latium region (Central Italy)

dc.contributor.authorFilippo, M.
dc.contributor.authorToro, Beniamino
dc.date.accessioned2018-11-27T18:07:03Z
dc.date.available2018-11-27T18:07:03Z
dc.date.issued1982-07
dc.descriptionInternational Symposium on the Activity of Oceanic Volcanoes. Ponta Delgada, 4-9 August 1980.en
dc.description.abstractGoing 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 referredĀ·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. […].en
dc.description.versioninfo:eu-repo/semantics/publishedVersionpt_PT
dc.identifier.citationFILIPPO, M.; TORO, B. (1982). Gravity residual anomalies and geothermics in Latium region (Central Italy). "Arquipélago. Série Ciências da Natureza", 3: 269-270.pt_PT
dc.identifier.urihttp://hdl.handle.net/10400.3/4889
dc.language.isoengpt_PT
dc.publisherUniversidade dos AƧorespt_PT
dc.subjectGeothermal Fieldsen
dc.subjectLatium Regionen
dc.subjectItalyen
dc.titleGravity residual anomalies and geothermics in Latium region (Central Italy)en
dc.typejournal article
dspace.entity.typePublication
oaire.citation.conferencePlacePonta Delgada, AƧorespt_PT
oaire.citation.endPage270pt_PT
oaire.citation.startPage269pt_PT
oaire.citation.titleArquipélago. Série Ciências da Naturezapt_PT
oaire.citation.volume3pt_PT
rcaap.rightsopenAccesspt_PT
rcaap.typearticlept_PT

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