Magmatic Iron Meteorite Petrogenesis: Partitioning of AG and Pd Between Solid and Liquid Metal

Details Magmatic Iron Meteorite Petrogenesis: Partitioning of AG and Pd Between Solid and Liquid Metal Magmatic Iron Meteorite Petrogenesis: Partitioning of AG and Pd Between Solid and Liquid Metal

Mar 1996

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1996lpi....27..199c&link_type=abstract

Lunar and Planetary Science, volume 27, page 199

Computer Science

1

Chronometer: Silver-Palladium, Experiments: Solid Metal/Liquid Metal Partitioning, Meteorites: Iron, Palladium: Partitioning Behavior, Silver: Partitioning Behavior

Scientific paper

Stimulated by new analytical data for the parent-daughter isotope system 107Pd/107Ag which appear to be inconsistent with the few laboratory determinations of partitioning behavior, we have carried out an experimental study of the partitioning of Ag and Pd between solid Fe-metal and S-bearing metallic liquid. Silver is incompatible in solid metal and partition coefficients decrease with increasing S-content in the metallic liquid. Palladium changes from modestly incompatible to modestly compatible in solid metal with increasing S-content in the metallic liquid. These new data are used to investigate Ag and Pd systematics in magmatic iron meteorites.

Affiliated with

Also associated with

No associations

Rating

Magmatic Iron Meteorite Petrogenesis: Partitioning of AG and Pd Between Solid and Liquid Metal 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 Iron Meteorite Petrogenesis: Partitioning of AG and Pd Between Solid and Liquid Metal, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Magmatic Iron Meteorite Petrogenesis: Partitioning of AG and Pd Between Solid and Liquid Metal will most certainly appreciate the feedback.

Rate now

Comments { 0 }

Profile ID: LFWR-SCP-O-1611359