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Geophysical exploration using gravity data

dc.contributor.advisorLedo Fernández, Juanjo
dc.contributor.authorOms Marin, Carla
dc.date.accessioned2019-10-03T14:23:07Z
dc.date.available2019-10-03T14:23:07Z
dc.date.issued2019-06
dc.descriptionTreballs Finals de Grau de Física, Facultat de Física, Universitat de Barcelona, Curs: 2019, Tutor: Juan Jose Ledo Fernándezca
dc.description.abstractThe geometry of the northern part of the Vallès fault, between La Garriga and Cànoves i Samalús is deduced from the gravimetric survey of the region. The survey consists of the relative measurement of the vertical gravitational acceleration with a gravimeter. From the readings acquired the residual anomaly is deduced to create a two-dimensional model of the section of the fault, approximating the bodies to different polygons with a characteristic densityca
dc.format.extent5 p.
dc.format.mimetypeapplication/pdf
dc.identifier.urihttps://hdl.handle.net/2445/141666
dc.language.isoengca
dc.rightscc-by-nc-nd (c) Oms, 2019
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessca
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.sourceTreballs Finals de Grau (TFG) - Física
dc.subject.classificationGravimetria (Geofísica)cat
dc.subject.classificationVallès (Catalunya)cat
dc.subject.classificationTreballs de fi de graucat
dc.subject.otherGravity measurementeng
dc.subject.otherVallèseng
dc.subject.otherBachelor's theseseng
dc.titleGeophysical exploration using gravity dataeng
dc.typeinfo:eu-repo/semantics/bachelorThesisca

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