Formation conditions of igneous regions in ordinary chondrites: Chico, Rose City, and other heavily shocked H and L chondrites
- 1 September 1997
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 102 (E9) , 21589-21611
- https://doi.org/10.1029/97je01873
Abstract
No abstract availableKeywords
This publication has 30 references indexed in Scilit:
- Chemical studies of H chondrites 8. On contemporary meteoroid streamsJournal of Geophysical Research, 1997
- Igneous inclusions from ordinary chondrites: High temperature cumulates and a shock meltJournal of Geophysical Research, 1994
- Evidence of Thermal Metamorphism on the C, G, B, and F AsteroidsScience, 1993
- Importance of considerations of mixing properties in establishing an internally consistent thermodynamic database: thermochemistry of minerals in the system Mg2SiO4-Fe2SiO4-SiO2Contributions to Mineralogy and Petrology, 1989
- A planetary, H-group pebble in the Barwell, L6, unshocked chondritic meteoriteEarth and Planetary Science Letters, 1988
- On the chondrite—achondrite transition: mineralogy and chemistry of Yamato 74160 (LL7)Earth and Planetary Science Letters, 1984
- Petrogenesis of complex veins in the Chantonnay (L6f) chondriteEarth and Planetary Science Letters, 1982
- Incipient melting in and shock classification of L-group chondritesEarth and Planetary Science Letters, 1979
- Apollo 14 inverted pigeonites: possible samples of lunar plutonic rocksEarth and Planetary Science Letters, 1972
- A Stony Meteorite from Washington County, Kan.Science, 1890