Please use this identifier to cite or link to this item:
http://hdl.handle.net/2122/5097
DC Field | Value | Language |
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dc.contributor.authorall | Gambetta, M..; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia | en |
dc.contributor.authorall | Aicardi, S. | en |
dc.contributor.authorall | Carmisciano, C.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia | en |
dc.contributor.authorall | Armadillo, E. | en |
dc.date.accessioned | 2009-06-24T11:31:52Z | en |
dc.date.available | 2009-06-24T11:31:52Z | en |
dc.date.issued | 2009 | en |
dc.identifier.uri | http://hdl.handle.net/2122/5097 | en |
dc.description.abstract | In this work we show the results of a resistivity tomography performed over the shallow part of a large cave system in the Mt.Armetta karst, Pennavaira valley northwestern Italy. The cave has been explored and surveyed by the authors themselves, thus a precise knowledge of size and shape of the subsurface voids is available. The cave, whose shallowest part exhibits narrow passages and large chambers, was developed in the Mesozoic sedimentary cover(Caprauna Armetta tectonic unit), an allochtonous nappe characterized by four deformation phases. The main target of the experiment is a region located at about 30 m below surface precisely spotted by ve 235m long ERT sections. Since cave develops in a windy summit area, the long-term stability of an eolic power plant tower, located over a karst void, is also considered. As a matter of fact, the footings of the eolic towers (approx 100 m high) may interfere with unpredictable shallow hollows, whose presence, in the power plant area, is more than likely. | en |
dc.language.iso | English | en |
dc.relation.ispartof | GEOITALIA2009 | en |
dc.subject | ERT | en |
dc.subject | VOID DETECTION | en |
dc.title | LARGE SUBSURFACE HOLLOWS REVEALED BY MEANS OF ELECTRICAL RESISTIVITY TOMOGRAPHY : THE CASE OF MT. ARMETTA KARST AREA, ITALY | en |
dc.type | Conference paper | en |
dc.description.status | Submitted | en |
dc.subject.INGV | 04. Solid Earth::04.02. Exploration geophysics::04.02.04. Magnetic and electrical methods | en |
dc.description.ConferenceLocation | Rimini | en |
dc.description.obiettivoSpecifico | 3.8. Geofisica per l'ambiente | en |
dc.description.fulltext | open | en |
dc.contributor.author | Gambetta, M.. | en |
dc.contributor.author | Aicardi, S. | en |
dc.contributor.author | Carmisciano, C. | en |
dc.contributor.author | Armadillo, E. | en |
dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia | en |
dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia | en |
item.openairetype | Conference paper | - |
item.cerifentitytype | Publications | - |
item.languageiso639-1 | en | - |
item.grantfulltext | open | - |
item.openairecristype | http://purl.org/coar/resource_type/c_18cf | - |
item.fulltext | With Fulltext | - |
crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma2, Roma, Italia | - |
crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma2, Roma, Italia | - |
crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma2, Roma, Italia | - |
crisitem.author.dept | UNIGE - Dipteris | - |
crisitem.author.orcid | 0000-0001-7357-2147 | - |
crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.classification.parent | 04. Solid Earth | - |
crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
Appears in Collections: | Conference materials |
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File | Description | Size | Format | |
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Abstract.pdf | 62.23 kB | Adobe PDF | View/Open |
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