Accretion temperature of the Tieschitz, H3, chondritic meteorite

Details Accretion temperature of the Tieschitz, H3, chondritic meteorite Accretion temperature of the Tieschitz, H3, chondritic meteorite

Jul 1979

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1979natur.280..116h&link_type=abstract

Nature, vol. 280, July 12, 1979, p. 116-119. Research supported by the Natural Environment Research Council.

Computer Science

22

Chemical Composition, Chondrites, Meteorites, Mineral Deposits, Planetary Evolution, Temperature Effects, Abundance, Crystallization, Czechoslovakia, Energy Spectra, Glass, Minerals, Phase Diagrams, Tieschitz Meteorite, Chondrules, Chondrites, Origin, Olivines, Pyroxenes, Composition, Petrology, Meteorites, Metamorphism, Volatiles, Silicates, Geochemistry, Electron Microscopy, Nepheline, Accretion, Fractional Crystallization, Pressure Gradients, Viscosity

Scientific paper

The Tieschitz, H3, chondritic meteorite apparently formed as part of a
parent-body by the accretion of both molten and solid materials with a
mean temperature of 800 + or - 100 C, followed by slow cooling to lower
temperatures. The data argue against the currently accepted model of
equilibration with a cooling gas of solar composition.

Affiliated with

Also associated with

No associations

Rating

Accretion temperature of the Tieschitz, H3, chondritic meteorite 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 Accretion temperature of the Tieschitz, H3, chondritic meteorite, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Accretion temperature of the Tieschitz, H3, chondritic meteorite will most certainly appreciate the feedback.

Rate now

Comments { 0 }

Profile ID: LFWR-SCP-O-1557487