A 3-D dynamic model for the anomalous topography and geoid over the south-east Indian Ridge
The anomalous sea-floor topography and geoid height over the Australian-Antarctic Discordance (AAD) are examined and attributed to dynamic mantle flow in this study. Because the subsidences of sea-floor depth and geoid with age exhibit forms of isostatic response of cooling from the surface, they ar...
Published in: | Geophysical Journal International |
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Main Authors: | , , |
Format: | Text |
Language: | English |
Published: |
Oxford University Press
1995
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Subjects: | |
Online Access: | http://gji.oxfordjournals.org/cgi/content/short/121/1/1 https://doi.org/10.1111/j.1365-246X.1995.tb03507.x |