Effect of oxygen partial pressure on the dislocation recovery in olivine: a new constraint on creep mechanisms

Details Effect of oxygen partial pressure on the dislocation recovery in olivine: a new constraint on creep mechanisms Effect of oxygen partial pressure on the dislocation recovery in olivine: a new constraint on creep mechanisms

Jul 1982

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1982pepi...28..312k&link_type=abstract

Physics of the Earth and Planetary Interiors, Volume 28, Issue 4, p. 312-319.

Physics

14

Scientific paper

The dislocation annihilation rate in experimentally deformed olivine single crystals was measured as a function of oxygen partial pressure (PO2). It was shown that the dislocation annihilation rate decreased with increasing PO2. This result is inconsistent with the reported PO2 dependence of creep rate (~ PO2+1/6) in single olivine crystals, thus indicating that the creep in single olivine crystals is not rate-controlled by recovery, under the experimentally investigated conditions.

Affiliated with

Also associated with

No associations

Rating

Effect of oxygen partial pressure on the dislocation recovery in olivine: a new constraint on creep mechanisms 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 Effect of oxygen partial pressure on the dislocation recovery in olivine: a new constraint on creep mechanisms, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Effect of oxygen partial pressure on the dislocation recovery in olivine: a new constraint on creep mechanisms will most certainly appreciate the feedback.

Rate now

Comments { 0 }

Profile ID: LFWR-SCP-O-1024477