Interpretation of the lithospheric structure beneath the Indian Ocean from gravity gradient data
Abstract
Global geoidal undulations are often used as the constraining parameter to model the mantle convection pattern, while gravity data are typically applied to interpret the lithospheric structure. In more recent studies, especially after launching the Gravity field and steady-state Ocean Circulation Explorer (GOCE) satellite gravity-gradiometry mission, gravity gradient measurements have also been used in various geoscience applications. The main...
Paper Details
Title
Interpretation of the lithospheric structure beneath the Indian Ocean from gravity gradient data
Published Date
Oct 1, 2019
Volume
183
Pages
103934 - 103934
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