Regional linear cross-strike discontinuities in Western Aphrodite Terra, Venus

Details Regional linear cross-strike discontinuities in Western Aphrodite Terra, Venus Regional linear cross-strike discontinuities in Western Aphrodite Terra, Venus

Jun 1987

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1987georl..14..607c&link_type=abstract

Geophysical Research Letters (ISSN 0094-8276), vol. 14, June 1987, p. 607-610.

Mathematics

Logic

29

Geological Faults, Planetary Geology, Structural Properties (Geology), Tectonics, Venus Surface, Discontinuity, Planetary Structure, Topography, Venus, Aphrodite Terra, Surface, Features, Topography, Highlands, Description, Characteristics, Comparisons, Tectonics, Radar Methods, Spacecraft Observations, Pioneer Venus Orbiter, Altimetry, Reflectivity, Imagery, Maps, Size, Length, Width, Formation, Origin, Hypotheses

Scientific paper

Western Aphrodite Terra, Venus, is characterized by a series of parallel linear structural discontinuities 2000 - 4000 km in length and 100 - 200 km wide, which strike at high angles to the general topographic trend of the highlands. The detailed characteristics of these features are similar to terrestrial oceanic fracture zones and strike-slip fault zones. Either interpretation implies the presence of large-scale horizontal tectonic movement on Venus.

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