Integrated geoelectrical and magnetotelluric exploration at Gran Sasso d'Italia range (Central Apennines)

We carried out three electrical soundings, with continuous polar dipole-dipole array, and three magnetotelluric stations at Gran Sasso d'Italia, in the area of Campo Imperatore. Geoelectrical data show the existence of a resistive background with exceptionally high values of resistivity (greate...

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Main Authors: A. Zaja, M. Giudici, L. Alfano
Format: Article
Language:English
Published: Istituto Nazionale di Geofisica e Vulcanologia (INGV) 1998-06-01
Series:Annals of Geophysics
Subjects:
Online Access:http://www.annalsofgeophysics.eu/index.php/annals/article/view/4348
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author A. Zaja
M. Giudici
L. Alfano
author_facet A. Zaja
M. Giudici
L. Alfano
author_sort A. Zaja
collection DOAJ
description We carried out three electrical soundings, with continuous polar dipole-dipole array, and three magnetotelluric stations at Gran Sasso d'Italia, in the area of Campo Imperatore. Geoelectrical data show the existence of a resistive background with exceptionally high values of resistivity (greater than 25000 ? m) at a depth of about 250 m. The magnetotelluric data were used to constrain the thickness of this resistive layer, below which we find an intermediate conductive structure and a deeper resistive background. The geological interpretation of this result is still open to discussion, but we can exclude that the shallow resistive layer consists of Cretaceous limestones, since their resistivity has been estimated to be about 5000 ? m.
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spelling doaj.art-849e4443c19645f78a28bad8debe7f422022-12-21T20:20:28ZengIstituto Nazionale di Geofisica e Vulcanologia (INGV)Annals of Geophysics1593-52132037-416X1998-06-0141310.4401/ag-4348Integrated geoelectrical and magnetotelluric exploration at Gran Sasso d'Italia range (Central Apennines)A. ZajaM. GiudiciL. AlfanoWe carried out three electrical soundings, with continuous polar dipole-dipole array, and three magnetotelluric stations at Gran Sasso d'Italia, in the area of Campo Imperatore. Geoelectrical data show the existence of a resistive background with exceptionally high values of resistivity (greater than 25000 ? m) at a depth of about 250 m. The magnetotelluric data were used to constrain the thickness of this resistive layer, below which we find an intermediate conductive structure and a deeper resistive background. The geological interpretation of this result is still open to discussion, but we can exclude that the shallow resistive layer consists of Cretaceous limestones, since their resistivity has been estimated to be about 5000 ? m.http://www.annalsofgeophysics.eu/index.php/annals/article/view/4348Magnetotelluricdipole-dipole DC soundingcrustal explorationCentral Apennines
spellingShingle A. Zaja
M. Giudici
L. Alfano
Integrated geoelectrical and magnetotelluric exploration at Gran Sasso d'Italia range (Central Apennines)
Annals of Geophysics
Magnetotelluric
dipole-dipole DC sounding
crustal exploration
Central Apennines
title Integrated geoelectrical and magnetotelluric exploration at Gran Sasso d'Italia range (Central Apennines)
title_full Integrated geoelectrical and magnetotelluric exploration at Gran Sasso d'Italia range (Central Apennines)
title_fullStr Integrated geoelectrical and magnetotelluric exploration at Gran Sasso d'Italia range (Central Apennines)
title_full_unstemmed Integrated geoelectrical and magnetotelluric exploration at Gran Sasso d'Italia range (Central Apennines)
title_short Integrated geoelectrical and magnetotelluric exploration at Gran Sasso d'Italia range (Central Apennines)
title_sort integrated geoelectrical and magnetotelluric exploration at gran sasso d italia range central apennines
topic Magnetotelluric
dipole-dipole DC sounding
crustal exploration
Central Apennines
url http://www.annalsofgeophysics.eu/index.php/annals/article/view/4348
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AT mgiudici integratedgeoelectricalandmagnetotelluricexplorationatgransassoditaliarangecentralapennines
AT lalfano integratedgeoelectricalandmagnetotelluricexplorationatgransassoditaliarangecentralapennines