Radial resolving power of far-field differential sea-level highstands in the inference of mantle viscosity

Details Radial resolving power of far-field differential sea-level highstands in the inference of mantle viscosity Radial resolving power of far-field differential sea-level highstands in the inference of mantle viscosity

Nov 2007

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2007geoji.171..881k&link_type=abstract

Geophysical Journal International, Volume 171, Issue 2, pp. 881-889.

Astronomy and Astrophysics

Astronomy

3

Inverse Problem, Mantle Viscosity, Sea Level

Scientific paper

For two decades leading to the late 1980s, the prevailing view from studies of glacial isostatic adjustment (GIA) data was that the viscosity of the Earth's mantle increased moderately, if at all, from the base of the lithosphere to the core-mantle boundary. This view was first questioned by Nakada & Lambeck, who argued that differential sea-level (DSL) highstands between pairs of sites in the Australian region preferred an increase of approximately two orders of magnitude from the mean viscosity of the upper to the lower mantle, in accord with independent inferences from observables related to mantle convection. We use non-linear Bayesian inference to provide the first formal resolving power analysis of the Australian DSL data set. We identify three radial regions, two within the upper mantle (110-270 km and 320-570 km depth) and one in the lower mantle (1225-2265 km depth), over which the average of viscosity is well constrained by the data. We conclude that: (1) the DSL data provide a resolution in the inference of upper mantle viscosity that is better than implied by forward analyses based on isoviscous regions above and below the 670 km depth discontinuity and (2) the data do not strongly constrain viscosity at either the base or top of the lower mantle. Finally, our inversions also quantify the significant bias that may be introduced in inversions of the DSL highstands that do not simultaneously estimate the thickness of the elastic lithosphere.

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