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Geophysical exploration using gravity data

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Treballs Finals de Grau de Física, Facultat de Física, Universitat de Barcelona, Curs: 2019, Tutor: Juan Jose Ledo Fernández

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The 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 density

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Geophysical exploration using gravity data