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Gravity inversion by means of growing bodies

dc.contributor.authorCamacho, AG, A.G.
dc.contributor.authorMontesinos, F. G.
dc.contributor.authorVieira, Ricardo
dc.date.accessioned2023-06-20T16:56:06Z
dc.date.available2023-06-20T16:56:06Z
dc.date.issued2000
dc.description.abstractThis paper presents a gravity inversion method for determining the volumes of bodies with pre-established density contrasts. The method works step-by-step on a prismatic partition of the subsurface volume, expanding the anomalous bodies to fit the observed gravity values in a systematic exploration of model possibilities. The process is treated in a 3-D context; at the same time, it can determine a simple regional trend. Moreover, positive and negative density contrasts are simultaneously accepted. The solution is obtained by a double condition: (1) the e(2)-fitness to the observed gravity data (model fitness) and (2) the minimization of the total (weighted) anomalous mass (model smoothness). A positive parameter is used to balance the two minimization terms. The method is applied to a simulated example and also to a real example: the volcanic island of Gran Canaria (Canary Islands, Spain). In both cases, the results obtained show the possibilities of the method.
dc.description.departmentUnidad Deptal. de Astronomía y Geodesia
dc.description.facultyFac. de Ciencias Matemáticas
dc.description.refereedTRUE
dc.description.statuspub
dc.eprint.idhttps://eprints.ucm.es/id/eprint/15992
dc.identifier.doi10.1190/1.1444729
dc.identifier.issn0016-8033
dc.identifier.officialurlhttp://geophysics.geoscienceworld.org/content/65/1/95.full.pdf+html
dc.identifier.relatedurlhttp://geophysics.geoscienceworld.org/
dc.identifier.urihttps://hdl.handle.net/20.500.14352/57460
dc.issue.number1
dc.journal.titleGeophysics
dc.language.isoeng
dc.page.final101
dc.page.initial95
dc.publisherSOC EXPLORATION GEOPHYSICISTS
dc.rights.accessRightsopen access
dc.subject.cdu550.3
dc.subject.keywordCanary-Islands
dc.subject.keywordGran-Canaria
dc.subject.keywordGeochemistry & Geophysics
dc.subject.ucmGeofísica
dc.subject.unesco2507 Geofísica
dc.titleGravity inversion by means of growing bodies
dc.typejournal article
dc.volume.number65
dcterms.referencesBosshard, E., and MacFarlane,D.J., 1970, Crustal structure of theWestern Canary Islands from seismic refraction and gravity data: J. Geophys. Res., 75, 4901–4918. Camacho, A. G., Montesinos, F. G., and Vieira, R., 1997, A threedimensional gravity inversion applied to Sao Miguel Island (Azores): J. Geophys. Res., 102, 7705–7715. Moritz, H., 1980, Advanced physical geodesy: HerbertWichmannVerlag. Pedersen, L. B., 1979, Constrained inversion of potential field data: Geophys. Prosp., 27, 726–748. Pérez-Torrado, F.J., Marti, J., Mangas, J., and Day, S., 1997, Ignimbrites of the Roque Nublo group, Gran Canaria, Canary Islands: Bull. Volcanol., 58, 647–654. Pick, M., Picha, J., and Vysk ˆ ocil,V., 1973, Theory of the Earth’s gravity field: Elsevier Science Publ. Co. René, R. M., 1986, Gravity inversion using open, reject, and “shapeof- anomaly” fill criteria: Geophysics, 51, 988–994. Rothman, D. H., 1985, Nonlinear inversion, statistical mechanics, and residual statics estimation: Geophysics, 50, 2784–2796. Silva, J.B.C. and Hohmann,G.W., 1983, Nonlinear magnetic inversion using a random search method: Geophysics, 46, 1645–1658. Tarantola, A., 1988, The inverse problem theory: Methods for data fitting and model parameter estimation: Elsevier Science Publ. Co. Zidarov, D., 1990, Inverse gravimetric problem in geoprospecting and geodesy: Elsevier Science Publ. Co.
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