The Geothermal Gradient of Io: Consequences for Lithosphere Structure and Volcanic Eruptive Activity

Details The Geothermal Gradient of Io: Consequences for Lithosphere Structure and Volcanic Eruptive Activity The Geothermal Gradient of Io: Consequences for Lithosphere Structure and Volcanic Eruptive Activity

Mar 2010

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2010lpi....41.1130l&link_type=abstract

41st Lunar and Planetary Science Conference, held March 1-5, 2010 in The Woodlands, Texas. LPI Contribution No. 1533, p.1130

Physics

Scientific paper

We re-evaluate Io's temperature structure with temperature-dependent
thermal parameters to find the depths at which sulphur volatiles, buried
by volcanic activity, melt to be mixed into later magmas, affecting
eruption rates and intrusion depths.

Affiliated with

Also associated with

No associations

Rating

The Geothermal Gradient of Io: Consequences for Lithosphere Structure and Volcanic Eruptive Activity 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 The Geothermal Gradient of Io: Consequences for Lithosphere Structure and Volcanic Eruptive Activity, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and The Geothermal Gradient of Io: Consequences for Lithosphere Structure and Volcanic Eruptive Activity will most certainly appreciate the feedback.

Rate now

Comments { 0 }

Profile ID: LFWR-SCP-O-885972