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On the applicability of joint inversion of gravity and resistivity data to the study of a tectonic sedimentary basin in Northern Portugal

dc.contributor.authorRepresa, Patrícia
dc.contributor.authorSantos, F. A. Monteiro
dc.contributor.authorRibeiro, Joana A.
dc.contributor.authorAfonso, A. Andrade
dc.contributor.authorRibeiro, José
dc.contributor.authorMoreira, Mário
dc.contributor.authorMendes-Victor, L. A.
dc.date.accessioned2016-03-18T15:00:34Z
dc.date.available2016-03-18T15:00:34Z
dc.date.issued2015-10
dc.description.abstractThe Chaves basin is a pull-apart tectonic depression implanted on granites, schists, and graywackes, and filled with a sedimentary sequence of variable thickness. It is a rather complex structure, as it includes an intricate network of faults and hydrogeological systems. The topography of the basement of the Chaves basin still remains unclear, as no drill hole has ever intersected the bottom of the sediments, and resistivity surveys suffer from severe equivalence issues resulting from the geological setting. In this work, a joint inversion approach of 1D resistivity and gravity data designed for layered environments is used to combine the consistent spatial distribution of the gravity data with the depth sensitivity of the resistivity data. A comparison between the results from the inversion of each data set individually and the results from the joint inversion show that although the joint inversion has more difficulty adjusting to the observed data, it provides more realistic and geologically meaningful models than the ones calculated by the inversion of each data set individually. This work provides a contribution for a better understanding of the Chaves basin, while using the opportunity to study further both the advantages and difficulties comprising the application of the method of joint inversion of gravity and resistivity data.pt_PT
dc.identifier.citationREPRESAS, Patrícia; [et al.] - On the applicability of joint inversion of gravity and resistivity data to the study of a tectonic sedimentary basin in Northern Portugal. Pure and Applied Geophysics. ISSN. 0033-4553. Vol. 172, N.º 10 (2015), pp. 2681-2699pt_PT
dc.identifier.doi10.1007/s00024-014-0920-xpt_PT
dc.identifier.issn0033-4553
dc.identifier.issn1420-9136
dc.identifier.urihttp://hdl.handle.net/10400.21/5915
dc.language.isoengpt_PT
dc.peerreviewedyespt_PT
dc.publisherSpringer Basel AGpt_PT
dc.relation.publisherversionhttp://link.springer.com/article/10.1007/s00024-014-0920-xpt_PT
dc.subjectJoint inversionpt_PT
dc.subjectGravity datapt_PT
dc.subjectResistivity datapt_PT
dc.subjectTectonic basinpt_PT
dc.subjectPortugalpt_PT
dc.titleOn the applicability of joint inversion of gravity and resistivity data to the study of a tectonic sedimentary basin in Northern Portugalpt_PT
dc.typejournal article
dspace.entity.typePublication
oaire.citation.endPage2699pt_PT
oaire.citation.issue10pt_PT
oaire.citation.startPage2681pt_PT
oaire.citation.volume172pt_PT
person.familyNameMoreira
person.givenNameMário
person.identifier2793313
person.identifier.ciencia-idA214-9FF2-5978
person.identifier.orcid0000-0002-5933-3681
person.identifier.ridI-1214-2015
person.identifier.scopus-author-id26538801900
rcaap.rightsclosedAccesspt_PT
rcaap.typearticlept_PT
relation.isAuthorOfPublication32d7ffa4-6692-421b-9d99-9571197bad17
relation.isAuthorOfPublication.latestForDiscovery32d7ffa4-6692-421b-9d99-9571197bad17

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