Geologic Evolution of the Martian Dichotomy and Plains Magnetization in the Ismenius Area of Mars

Details Geologic Evolution of the Martian Dichotomy and Plains Magnetization in the Ismenius Area of Mars Geologic Evolution of the Martian Dichotomy and Plains Magnetization in the Ismenius Area of Mars

Mar 2004

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2004lpi....35.2117s&link_type=abstract

35th Lunar and Planetary Science Conference, March 15-19, 2004, League City, Texas, abstract no.2117

Mathematics

Logic

Scientific paper

Analysis of the geologic history indicates that the 2.5 km of relief is
a primary feature, and that the boundary may have experienced
relaxation. Gravity and magnetic anomalies suggest the possible presence
of fossil magmatic intrusions at depth.

Affiliated with

Also associated with

No associations

Rating

Geologic Evolution of the Martian Dichotomy and Plains Magnetization in the Ismenius Area of Mars 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 Geologic Evolution of the Martian Dichotomy and Plains Magnetization in the Ismenius Area of Mars, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Geologic Evolution of the Martian Dichotomy and Plains Magnetization in the Ismenius Area of Mars will most certainly appreciate the feedback.

Rate now

Comments { 0 }

Profile ID: LFWR-SCP-O-1643276