Recrystallized chondrules in the Sharps (H-3) chondrite

Details Recrystallized chondrules in the Sharps (H-3) chondrite Recrystallized chondrules in the Sharps (H-3) chondrite

Oct 1968

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1968gecoa..32.1111d&link_type=abstract

Geochimica et Cosmochimica Acta, vol. 32, Issue 10, pp.1111-1116

Computer Science

5

Scientific paper

Microprobe analyses of fifty chondrules in the Sharps (H-3) chondrite showed three to contain essentially homogeneous, calcium-poor olivines. All three show textural evidence of recrystallization, which is subtle in two and pronounced in one. It is concluded that these chondrules were recrystallized before they entered Sharps. Although Sharps is an H-group chondrite, the recrystallized chondrules have olivine and pyroxene compositions appropriate to recrystallized LL-group chondrites. They thus suggest that low-iron material, with a complex previous history, was present at the place of formation of the H-group chondrites.

Affiliated with

Also associated with

No associations

Rating

Recrystallized chondrules in the Sharps (H-3) chondrite 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 Recrystallized chondrules in the Sharps (H-3) chondrite, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Recrystallized chondrules in the Sharps (H-3) chondrite will most certainly appreciate the feedback.

Rate now

Comments { 0 }

Profile ID: LFWR-SCP-O-1844600