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Localization of gravity and topography: constraints on the tectonics and mantle dynamics of Venus

Simons, Mark and Solomon, Sean C. and Hager, Bradford H. (1997) Localization of gravity and topography: constraints on the tectonics and mantle dynamics of Venus. Geophysical Journal International, 131 (1). pp. 24-44. ISSN 0956-540X. https://resolver.caltech.edu/CaltechAUTHORS:20130710-142207254

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Abstract

We develop a method for spatio-spectral localization of harmonic data on a sphere and use it to interpret recent high-resolution global estimates of the gravity and topography of Venus in the context of geodynamical models. Our approach applies equally to the simple spatial windowing of harmonic data and to variable-length-scale analyses, which are analogous to a wavelet transform in the Cartesian domain. Using the variable-length-scale approach, we calculate the localized RMS amplitudes of gravity and topography, as well as the spectral admittance between the two fields, as functions of position and wavelength. The observed admittances over 10 per cent of the surface of Venus (highland plateaus and tessera regions) are consistent with isostatic compensation of topography by variations in crustal thickness, while admittances over the remaining 90 per cent of the surface (rises, plains and lowlands) indicate that long-wavelength topography is dominantly the result of vertical convective tractions at the base of the lithosphere. The global average crustal thickness is less than 30 km, but can reach values as large as 40 km beneath tesserae and highland plateaus. We also note that an Earth-like radial viscosity structure cannot be rejected by the gravity and topography data and that, without a mechanical model of the lithosphere, admittance values cannot constrain the thickness of the thermal boundary layer of Venus. Modelling the lithosphere as a thin elastic plate indicates that at the time of formation of relief in highland plateaus and tesserae, the effective elastic plate thickness, T_e, was less than 20 km. Estimates of T_e at highland rises are consistently less than 30 km. Our inability to find regions with T_e > 30 km is inconsistent with predictions made by a class of catastrophic resurfacing models.


Item Type:Article
Related URLs:
URLURL TypeDescription
http://dx.doi.org/10.1111/j.1365-246X.1997.tb00593.x DOIUNSPECIFIED
http://gji.oxfordjournals.org/content/131/1/24PublisherUNSPECIFIED
ORCID:
AuthorORCID
Simons, Mark0000-0003-1412-6395
Hager, Bradford H.0000-0002-5643-1374
Additional Information:© 1997 RAS. Received March 10, 1997. Accepted April 24, 1997. We thank Alex Konopliv and Bill Sjogren for distributing their Venus gravity model before publication. We have benefitted from discussions with Ming Fang, Tom Jordan, Patrick McGovern, Noriyuki Namiki and Svetlana Panasyuk, as well as from thorough reviews by Catherine Johnson and Roger Phillips. This research was supported by NASA grants NAGW-2161, NAGW-3276, NAGW-3425 and NAG5-4077, and NSF grant EAR-9506427.
Funders:
Funding AgencyGrant Number
NASANAGW-2161
NASANAGW-3276
NASANAGW-3425
NASANAG5-4077
NSFEAR-9506427
Subject Keywords:convection, geoid, gravity, tectonics, Venus, wavelets
Issue or Number:1
Record Number:CaltechAUTHORS:20130710-142207254
Persistent URL:https://resolver.caltech.edu/CaltechAUTHORS:20130710-142207254
Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:39290
Collection:CaltechAUTHORS
Deposited By: Tony Diaz
Deposited On:20 Sep 2013 19:54
Last Modified:09 Mar 2020 13:18

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