High-temperature condensates in chondrites and the environment in which they formed

Computer Science

Scientific paper

Rate now

  [ 0.00 ] – not rated yet Voters 0   Comments 0

Details

10

Scientific paper

Chemical compositions of melilitee and titaniferous pyroxenes in calcium- and aluminum-rich inclusions in carbonaceous chondrites are consistent with their origin as hightemperature condensates from a gas of solar composition. Thermodynamic calculations indicate that the highest temperature minerals equilibrated with the gas at temperatures in excess of 1400°K. The lack of evidence for direct condensation of gas to liquid enables us to set an upper limit to the pressure when the inclusions formed which may be as low as 2.2 × 10 -3 atm . Glasses, which are commonly found in chondrules, are interpreted as quench products of liquids formed by secondary reheating of primary solid condensates. The high-temperature inclusions constitute evidence that accretion of grains to cm-sized objects occurred at a very early stage in the evolution of the solar nebula.

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

High-temperature condensates in chondrites and the environment in which they formed 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 High-temperature condensates in chondrites and the environment in which they formed, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and High-temperature condensates in chondrites and the environment in which they formed will most certainly appreciate the feedback.

Rate now

     

Profile ID: LFWR-SCP-O-1637589

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