Rheological Properties of Late-Stage Lava Flows on Ascraeus Mons: New Evidence from HRSC

Details Rheological Properties of Late-Stage Lava Flows on Ascraeus Mons: New Evidence from HRSC Rheological Properties of Late-Stage Lava Flows on Ascraeus Mons: New Evidence from HRSC

Mar 2005

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2005lpi....36.1727h&link_type=abstract

36th Annual Lunar and Planetary Science Conference, March 14-18, 2005, in League City, Texas, abstract no.1727

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Scientific paper

We report on estimates of the rheological properties of late-stage lava
flows on the eastern flank of Ascraeus Mons, Mars, using HRSC data; we
conclude that the lava flows investigated are likely to be basaltic to
andesitic in composition.

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