A method of calculating lithosphere thickness from observations of deglacial land uplift and tilt

dc.contributor.authorWolf, Detlefde
dc.date.accessioned2010-02-08de
dc.date.accessioned2016-03-31T11:42:03Z
dc.date.available2010-02-08de
dc.date.available2016-03-31T11:42:03Z
dc.date.issued1986de
dc.description.abstractThe study proposes an inversion method applicable to observations of deglacial land uplift and tilt near the margin of a major Pleistocene ice-sheet. This information allows the determination of the cross-section of the ice-sheet and the calculation of the thickness of the lithosphere. The method is applied to the Pleistocene glaciations in Fennoscandia and Laurentia and yields similar lithosphere thicknesses of 110 ± 30 km and 130 ± 35 km, respectively. Since the method is based on a static theoretical model, the thicknesses must be interpreted as upper bounds.en
dc.identifier.other321600290de
dc.identifier.urihttp://nbn-resolving.de/urn:nbn:de:bsz:93-opus-50867de
dc.identifier.urihttp://elib.uni-stuttgart.de/handle/11682/7149
dc.identifier.urihttp://dx.doi.org/10.18419/opus-7132
dc.language.isoende
dc.rightsinfo:eu-repo/semantics/openAccessde
dc.subject.classificationLithosphäre , Isostasie , Fennoskandia , Platte <Geologie>de
dc.subject.ddc550de
dc.titleA method of calculating lithosphere thickness from observations of deglacial land uplift and tilten
dc.typearticlede
ubs.fakultaetFakultätsübergreifend / Sonstige Einrichtungde
ubs.institutSonstige Einrichtungde
ubs.opusid5086de
ubs.publikation.sourceJournal of geophysics 60 (1986), S. 28-32de
ubs.publikation.typZeitschriftenartikelde

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