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dc.contributor.authorRiller, Ulrich
dc.contributor.authorGötze, Hans-Joachim
dc.contributor.authorSchmidt, Sabine
dc.contributor.authorTrumbull, Robert
dc.contributor.authorHongn, Fernado
dc.contributor.authorPetrinovic, Ivan
dc.contributor.editorPhilipp, Sonja
dc.contributor.editorLeiss, Bernd
dc.contributor.editorVollbrecht, Axel
dc.contributor.editorTanner, David
dc.contributor.editorGudmundsson, Agust
dc.date.accessioned2010-11-26T13:21:34Z
dc.date.accessioned2013-01-28T10:20:24Z
dc.date.available2010-11-26T13:21:34Z
dc.date.available2013-01-28T10:20:24Z
dc.date.issued2006-03
dc.identifier.citationPhilipp, S.; Leiss, B; Vollbrecht, A.; Tanner, D.; Gudmundsson, A. (eds.): 11. Symposium "Tektonik, Struktur- und Kristallingeologie"; 2006, Univ.-Verl. Göttingen, p. 181 - 182.
dc.identifier.isbn3-938616-40-7
dc.identifier.urihttp://hdl.handle.net/11858/00-1735-0000-0001-3475-2
dc.description.abstractStructural analysts are often faced with the problem of identifying prominent structural discontinuities covered by post-tectonic sedimentary or volcanic rocks. Gravity fields are often used to delineate the trace of buried discontinuities but are frequently found to be too crude to localize discontinuities adequately. Here, we introduce the importance of dip curvature of the isostatic residual gravity for identifying upper-crustal discontinuities. The relationship between Bouguer gravity, isostatic residual gravity and its dip curvature, first-order structural elements and distribution of Neogene volcanic rocks was examined in the central Andean plateau, more specifically, the southern Altiplano and the Puna...
dc.format.mimetypeapplication/pdf
dc.language.isodeu
dc.publisherUniversitätsverlag Göttingen
dc.relation.ispartof11. Symposium "Tektonik, Struktur- und Kristallingeologie"
dc.subject.ddc551
dc.subject.gokTSX 000
dc.subject.gokTQA 000
dc.subject.gokVAE 811
dc.subject.gokVEX 100
dc.titleIdentification of uppercrustal discontinuities using dip curvature analysis of isostatic residual gravity: examples from the central Andes
dc.typeanthologyArticle
dc.subject.gokverbalSüdamerika {Geophysik}
dc.subject.gokverbalGravimetrische Verfahren {Geophysik}
dc.subject.gokverbalAlpidische Orogene {Geologie}
dc.subject.gokverbalAnden {Geologie}
dc.bibliographicCitation.firstPage181
dc.bibliographicCitation.lastPage182
dc.identifier.doi10.23689/fidgeo-1887
dc.type.versionpublishedVersion
dc.subject.freeZentralanden
dc.subject.freeErdkruste
dc.subject.freeDiskontinuität <Geologie>
dc.subject.freeGravimetrie
dc.relation.collectionGeologische Wissenschaften
dc.description.typeconference


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