Measurement of Tectonic Strain Based on Crater Elongations: an Improved Technique Applied to Tempe Terra, Mars

Mathematics – Logic

Scientific paper

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Craters, Extension, Mars, Strain, Tempe Terra

Scientific paper

Dozens of elongated craters in the Tharsis region of Mars clearly appear to be deformed by normal faults and grabens. Thus, elongated craters should provide a useful tool in the quantitative estimation of strain. In practice, however, several factors make this technique problematic, including (1) non-tectonic processes and structural controls may produce elongated craters upon and (or) following impact; (2) strain estimates must deal with averaging individual strain vectors of varying magnitude, trend, location, and age; and (3) tectonic strain varies in trend and magnitude as a function of age and location. Given these factors, a careful approach should be taken to adjust for non-tectonic elongations and to minimize the effects of geologic variables when estimating tectonic strain from crater elongations.

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