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A comparison of three gravity inversion methods for crustal thickness modelling in Tibet plateau
KTH, School of Architecture and the Built Environment (ABE), Urban Planning and Environment, Geoinformatik och Geodesi.
2012 (English)In: Journal of Asian Earth Sciences, ISSN 1367-9120, E-ISSN 1878-5786, Vol. 43, no 1, 89-97 p.Article in journal (Refereed) Published
Abstract [en]

Crustal thickness can be determined by gravimetric methods based on different assumptions, e.g. by isostatic hypotheses. Here we compare three gravimetric inversion methods to estimate the Moho depth. Two Moho models based on the Vening Meinesz-Moritz hypothesis and one by using Parker-Oldenburg's algorithm, which are investigated in Tibet plateau. The results are compared with CRUST2.0, and it will be presented that the estimated Moho depths from the Vening Meinesz-Moritz model will be better than the Parker-Oldenburg's algorithm.

Place, publisher, year, edition, pages
2012. Vol. 43, no 1, 89-97 p.
Keyword [en]
Inversion method, Isostasy, Moho depth, Mohorovicic discontinuity, Parker-Oldenburg's algorithm, Vening Meinesz-Moritz hypothesis
National Category
Earth and Related Environmental Sciences
Identifiers
URN: urn:nbn:se:kth:diva-58812DOI: 10.1016/j.jseaes.2011.08.013ISI: 000297881500007Scopus ID: 2-s2.0-82855172108OAI: oai:DiVA.org:kth-58812DiVA: diva2:474558
Note
QC 20120109Available from: 2012-01-09 Created: 2012-01-09 Last updated: 2017-12-08Bibliographically approved

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  • apa
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  • Other locale
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