Silica-rich Igneous Rims Around Magnesian Chondrules in CR Carbonaceous Chondrites: Evidence for Fractional Condensation During Chondrule Formation

Details Silica-rich Igneous Rims Around Magnesian Chondrules in CR Carbonaceous Chondrites: Evidence for Fractional Condensation During Chondrule Formation Silica-rich Igneous Rims Around Magnesian Chondrules in CR Carbonaceous Chondrites: Evidence for Fractional Condensation During Chondrule Formation

Mar 2003

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2003lpi....34.1451k&link_type=abstract

34th Annual Lunar and Planetary Science Conference, March 17-21, 2003, League City, Texas, abstract no.1451

Computer Science

3

Scientific paper

Type I chondrules in CRs are surrounded by silica-rich igneous rims
which may have formed by gas-solid condensation of SiO2-rich materials
onto chondrule surfaces and subsequent incomplete melting, or by direct
SiO condensation into chondrule melts.

Affiliated with

Also associated with

No associations

Rating

Silica-rich Igneous Rims Around Magnesian Chondrules in CR Carbonaceous Chondrites: Evidence for Fractional Condensation 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 Silica-rich Igneous Rims Around Magnesian Chondrules in CR Carbonaceous Chondrites: Evidence for Fractional Condensation During Chondrule Formation, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Silica-rich Igneous Rims Around Magnesian Chondrules in CR Carbonaceous Chondrites: Evidence for Fractional Condensation During Chondrule Formation will most certainly appreciate the feedback.

Rate now

Comments { 0 }

Profile ID: LFWR-SCP-O-1007788