Ledo Fernández, JuanjoOms Marin, Carla2019-10-032019-10-032019-06https://hdl.handle.net/2445/141666Treballs Finals de Grau de Física, Facultat de Física, Universitat de Barcelona, Curs: 2019, Tutor: Juan Jose Ledo FernándezThe 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 density5 p.application/pdfengcc-by-nc-nd (c) Oms, 2019http://creativecommons.org/licenses/by-nc-nd/3.0/es/Gravimetria (Geofísica)Vallès (Catalunya)Treballs de fi de grauGravity measurementVallèsBachelor's thesesinfo:eu-repo/semantics/bachelorThesisinfo:eu-repo/semantics/openAccess