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dc.contributor.authorHeinbockel, Raffaela Esther
dc.date.accessioned2010-10-12T19:29:42Z
dc.date.available2010-10-12T19:29:42Z
dc.date.issued2002
dc.identifier.urihttp://hdl.handle.net/11858/00-1735-0000-0001-3213-C
dc.description.abstractThis work presents the first three-dimensional gravity and magnetic investigation along the convergent Peruvian margin. Three-dimensional magnetic modelling is still a relatively untried and challenging technique. The gravity and magnetic models image nearly the whole margin which has been only partly resolved with geophysical methods up to now. The gravity and magnetic models are constructed for three areas between 7.25ʿS and 16.75ʿS and are based on the available wide-angle seismic velocity models (Hampel et al., 2002a; Broser et al., 2002). The continental margin is characterised by positive free-air anomalies of varying amplitudes, indicating that the margin has been shaped by the subduction of different features on the Nazca Plate...
dc.format.mimetypeapplication/pdf
dc.language.isoeng
dc.publisherUniv. Hamburg
dc.rights.urihttp://e-docs.geo-leo.de/rights
dc.subject.ddc551.1
dc.subject.ddc622.15
dc.subject.ddc550
dc.subject.gokTSX 800
dc.subject.gokTQA 000
dc.subject.gokTQB 000
dc.subject.gokVAE 880
dc.subject.gokVEX 800
dc.titleGravity and magnetic investigations along the Peruvian continental margin
dc.typemonograph
dc.subject.gokverbalPeru und Ecuador {Geophysik}
dc.subject.gokverbalGravimetrische Verfahren {Geophysik}
dc.subject.gokverbalErdmagnetische Verfahren {Geophysik}
dc.subject.gokverbalPassive und aktive Kontinentalränder {Geologie}
dc.subject.gokverbalPeru und Ecuador {Geologie}
dc.identifier.doi10.23689/fidgeo-387
dc.identifier.ppn361541120
dc.type.versionpublishedVersion
dc.relation.collectionGeophysik
dc.description.typethesis


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