The Effect of Large Melt Fraction on the Deformation Behavior of Peridotite: Implications for the Rheology of Io's Mantle

Details The Effect of Large Melt Fraction on the Deformation Behavior of Peridotite: Implications for the Rheology of Io's Mantle The Effect of Large Melt Fraction on the Deformation Behavior of Peridotite: Implications for the Rheology of Io's Mantle

Mar 2004

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2004lpi....35.1304s&link_type=abstract

35th Lunar and Planetary Science Conference, March 15-19, 2004, League City, Texas, abstract no.1304

Computer Science

2

Scientific paper

We measured the strength of partially molten peridotites with melt
contents > 10%. For a sample of olivine + 25 vol% MORB deformed in
compression at 1498 K and 1523 K and 300 MPa, we calculated a viscosity
of 5 × 10^15 Pa-s for 1 mm olivine grains.

Affiliated with

Also associated with

No associations

Rating

The Effect of Large Melt Fraction on the Deformation Behavior of Peridotite: Implications for the Rheology of Io's Mantle 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 Effect of Large Melt Fraction on the Deformation Behavior of Peridotite: Implications for the Rheology of Io's Mantle, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and The Effect of Large Melt Fraction on the Deformation Behavior of Peridotite: Implications for the Rheology of Io's Mantle will most certainly appreciate the feedback.

Rate now

Comments { 0 }

Profile ID: LFWR-SCP-O-1135866