Publication
Gravity residual anomalies and geothermics in Latium region (Central Italy)
dc.contributor.author | Filippo, M. | |
dc.contributor.author | Toro, Beniamino | |
dc.date.accessioned | 2018-11-27T18:07:03Z | |
dc.date.available | 2018-11-27T18:07:03Z | |
dc.date.issued | 1982-07 | |
dc.description | International Symposium on the Activity of Oceanic Volcanoes. Ponta Delgada, 4-9 August 1980. | en |
dc.description.abstract | 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 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. [ā¦]. | en |
dc.description.version | info:eu-repo/semantics/publishedVersion | pt_PT |
dc.identifier.citation | FILIPPO, 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.uri | http://hdl.handle.net/10400.3/4889 | |
dc.language.iso | eng | pt_PT |
dc.publisher | Universidade dos AƧores | pt_PT |
dc.subject | Geothermal Fields | en |
dc.subject | Latium Region | en |
dc.subject | Italy | en |
dc.title | Gravity residual anomalies and geothermics in Latium region (Central Italy) | en |
dc.type | journal article | |
dspace.entity.type | Publication | |
oaire.citation.conferencePlace | Ponta Delgada, AƧores | pt_PT |
oaire.citation.endPage | 270 | pt_PT |
oaire.citation.startPage | 269 | pt_PT |
oaire.citation.title | Arquipélago. Série Ciências da Natureza | pt_PT |
oaire.citation.volume | 3 | pt_PT |
rcaap.rights | openAccess | pt_PT |
rcaap.type | article | pt_PT |