Obliquity-related Ice Deposition in the Glaciated Martian Crater Greg, and Progress on Crater Chronometry

Details Obliquity-related Ice Deposition in the Glaciated Martian Crater Greg, and Progress on Crater Chronometry Obliquity-related Ice Deposition in the Glaciated Martian Crater Greg, and Progress on Crater Chronometry

Oct 2011

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2011epsc.conf.1394h&link_type=abstract

EPSC-DPS Joint Meeting 2011, held 2-7 October 2011 in Nantes, France. http://meetings.copernicus.org/epsc-dps2011, p.1394

Mathematics

Logic

Scientific paper

Crater count chronometry continues to be a valuable tool in interpreting Martian surface history and geological processes. We apply this and other techniques to analyze the important crater, Greg, east of Hellas. We present a new technique to discuss ages of strata and geological processes as a function of depth. Topography in the upper meters of Greg is controlled by obliquity-driven climatic episodes producing ice-rich mantles, and modulated by the solar longitude of perihelion.

Affiliated with

Also associated with

No associations

Rating

Obliquity-related Ice Deposition in the Glaciated Martian Crater Greg, and Progress on Crater Chronometry does not yet have a rating. At this time, there are no reviews or comments for this scientific paper.

If you have personal experience with Obliquity-related Ice Deposition in the Glaciated Martian Crater Greg, and Progress on Crater Chronometry, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Obliquity-related Ice Deposition in the Glaciated Martian Crater Greg, and Progress on Crater Chronometry will most certainly appreciate the feedback.

Rate now

Comments { 0 }

Profile ID: LFWR-SCP-O-1484683