Formation conditions of pyroxene-olivine and magnesian olivine chondrules
- 1 December 1990
- journal article
- Published by Elsevier in Geochimica et Cosmochimica Acta
- Vol. 54 (12) , 3475-3490
- https://doi.org/10.1016/0016-7037(90)90299-z
Abstract
No abstract availableThis publication has 24 references indexed in Scilit:
- Temperature conditions for chondrule formationMeteoritics, 1990
- Compositions and textures of relic forsterite in carbonaceous and unequilibrated ordinary chondritesGeochimica et Cosmochimica Acta, 1986
- Determination of major, trace and rare-earth elements in rocks by DCP—AESChemical Geology, 1985
- On the formation of meteoritic chondrules by aerodynamic drag heating in the solar nebulaEarth and Planetary Science Letters, 1984
- Evidence for secondary origin of chondrulesNature, 1981
- RELATIVE ABUNDANCES OF CHONDRULE PRIMARY TEXTURAL TYPES IN ORDINARY CHONDRITES AND THEIR BEARING ON CONDITIONS OF CHONDRULE FORMATIONMeteoritics, 1981
- Experimental reproduction of textures of chondrulesEarth and Planetary Science Letters, 1980
- Volatiles in chainpur chondrulesGeophysical Research Letters, 1979
- Compositions of droplet chondrules in the Manych (L-3) chondrite and the origin of chondrulesEarth and Planetary Science Letters, 1978
- The composition and origin of large microporphyritic chondrules in the Manych (L-3) chondriteEarth and Planetary Science Letters, 1978