Gradients in extension and strain at Beta Regio, Venus

Details Gradients in extension and strain at Beta Regio, Venus Gradients in extension and strain at Beta Regio, Venus

Mar 1997

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1997lpi....28.1153r&link_type=abstract

Conference Paper, 28th Annual Lunar and Planetary Science Conference, p. 153.

Mathematics

Logic

Venus Surface, Planetary Mantles, Topography, Geological Faults, Strain Distribution, Planetary Craters, Highlands, Volcanoes, Strain Measurement

Scientific paper

Magellan altimetry data have been used to quantify the rift topography of the Beta Regio highlands of Venus, taking profiles across the axes of all three major rifts at 50-km intervals. By assuming that vertical offsets in topography are caused by normal faulting, the altimetry difference along each profile can be used to estimate the extension across the rift.

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