Magmatic Dikes and Megafloods: A Protracted History of Interactions Between Magma and Subsurface Ice, Cerberus Fossae, Mars

Details Magmatic Dikes and Megafloods: A Protracted History of Interactions Between Magma and Subsurface Ice, Cerberus Fossae, Mars Magmatic Dikes and Megafloods: A Protracted History of Interactions Between Magma and Subsurface Ice, Cerberus Fossae, Mars

Mar 2010

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2010lpi....41.1271k&link_type=abstract

41st Lunar and Planetary Science Conference, held March 1-5, 2010 in The Woodlands, Texas. LPI Contribution No. 1533, p.1271

Physics

Scientific paper

A protracted period of dike intrusion away from Elysium Mons, Mars,
resulted in a segmented fracture system (Cerberus Fossae) that induced
multiple megafloods as intruding magma interacted with subsurface ice.

Affiliated with

Also associated with

No associations

Rating

Magmatic Dikes and Megafloods: A Protracted History of Interactions Between Magma and Subsurface Ice, Cerberus Fossae, 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 Magmatic Dikes and Megafloods: A Protracted History of Interactions Between Magma and Subsurface Ice, Cerberus Fossae, Mars, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Magmatic Dikes and Megafloods: A Protracted History of Interactions Between Magma and Subsurface Ice, Cerberus Fossae, Mars will most certainly appreciate the feedback.

Rate now

Comments { 0 }

Profile ID: LFWR-SCP-O-886605