Oxygen Isotopes of Chondrules in the Queen Alexandra Range 99177 CR3 Chondrite: Further Evidence for Systematic Relationships Between Chondrule Mg# and Δ^1^7O and the Role of Ice During Chondrule Formation

Physics

Scientific paper

Rate now

  [ 0.00 ] – not rated yet Voters 0   Comments 0

Details

1

Scientific paper

QUE 99177 chondrules steadily rise in Δ^1^7O (-5 to -1
‰) as Mg# decreases (99 to 97). Addition of +Δ1^7O H_2O ice
to dry precursors could reduce chondrule Mg# (by oxidation during
formation) while increasing Δ^1^7O. Estimated H_2O ice
Δ^1^7O is 0.5 to 6‰.

No associations

LandOfFree

Say what you really think

Search LandOfFree.com for scientists and scientific papers. Rate them and share your experience with other people.

Rating

Oxygen Isotopes of Chondrules in the Queen Alexandra Range 99177 CR3 Chondrite: Further Evidence for Systematic Relationships Between Chondrule Mg# and Δ^1^7O and the Role of Ice During Chondrule Formation 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 Oxygen Isotopes of Chondrules in the Queen Alexandra Range 99177 CR3 Chondrite: Further Evidence for Systematic Relationships Between Chondrule Mg# and Δ^1^7O and the Role of Ice During Chondrule Formation, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Oxygen Isotopes of Chondrules in the Queen Alexandra Range 99177 CR3 Chondrite: Further Evidence for Systematic Relationships Between Chondrule Mg# and Δ^1^7O and the Role of Ice During Chondrule Formation will most certainly appreciate the feedback.

Rate now

     

Profile ID: LFWR-SCP-O-1041285

  Search
All data on this website is collected from public sources. Our data reflects the most accurate information available at the time of publication.