Please use this identifier to cite or link to this item: http://dr.iiserpune.ac.in:8080/xmlui/handle/123456789/1209
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dc.contributor.authorBANERJEE, ARGHAen_US
dc.contributor.authorShirsat, Tejalen_US
dc.contributor.authorKumari, Reshamaen_US
dc.date.accessioned2018-10-05T05:11:15Z
dc.date.available2018-10-05T05:11:15Z
dc.date.issued2018-07en_US
dc.identifier.citationJournal of Geophysical Research-Earth Surface. Vol. 123(8).en_US
dc.identifier.issn2169-9011en_US
dc.identifier.urihttp://dr.iiserpune.ac.in:8080/xmlui/handle/123456789/1209
dc.identifier.urihttps://doi.org/10.1029/2018JF004621en_US
dc.description.abstractAn analysis of elevation data from several great escarpment regions across the globe revealed a prevalence of inverse power law forms among the escarpment profiles. The best fit power law exponent varies among profiles and has a global median value of 0.9 and standard deviation of 1.8. The power law form is consistent with the shape of a detachment-limited escarpment that is retreating headward while maintaining a constant shape. Such a constant-shape evolution requires the local denudation rate to be equal to the product of escarpment retreat rate and local slope. The available basin-averaged denudation rate data from several great escarpment regions are consistent with this constraint, and this allows estimation of the recent retreat rates of the escarpments within the constant-shape assumption.en_US
dc.language.isoenen_US
dc.publisherAmerican Geophysical Unionen_US
dc.subjectTOC-SEP-2018en_US
dc.subject2018en_US
dc.titlePrevalence of Power Law Profiles in Passive Margin Escarpmentsen_US
dc.typeArticleen_US
dc.contributor.departmentDept. of Earth and Climate Scienceen_US
dc.identifier.sourcetitleJournal of Geophysical Research-Earth Surfaceen_US
dc.publication.originofpublisherForeignen_US
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