Rambaldi, E. R. and Rajan, R. S. and Murrell, M. T. and Burnett, D. S. (1984) Coexisting Chalcophile and Lithophile Uranium in Qingzhen (EH3) Chondrite. Meteoritics, 19 (4). p. 295. ISSN 0026-1114. https://resolver.caltech.edu/CaltechAUTHORS:20150427-121135999
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Abstract
Mineralogical and textural studies of Qingzhen have shown that it is highly unequilibrated and that it contains a population of chondrules and isolated enstatite grains which preserve the record of more oxidizing nebular conditions (Rambaldi et al., 1983, 1984). Even though in the majority of cases these objects have been affected by various degrees of reduction, some still contain silicates with high (up to 10%) FeO contents.
| Item Type: | Article | ||||||
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| Additional Information: | © 1984 Meteoritical Society. Provided by the Nasa Astrophysics Data System. | ||||||
| Issue or Number: | 4 | ||||||
| Record Number: | CaltechAUTHORS:20150427-121135999 | ||||||
| Persistent URL: | https://resolver.caltech.edu/CaltechAUTHORS:20150427-121135999 | ||||||
| Official Citation: | Coexisting Chalcophile and Lithophile Uranium in Qingzhen (EH3) Chondrite Rambaldi, E. R.; Rajan, R. S.; Murrell, M. T.; Burnett, D. S. Meteoritics, Vol. 19, p.295 12/1984 | ||||||
| Usage Policy: | No commercial reproduction, distribution, display or performance rights in this work are provided. | ||||||
| ID Code: | 57010 | ||||||
| Collection: | CaltechAUTHORS | ||||||
| Deposited By: | Ruth Sustaita | ||||||
| Deposited On: | 27 Apr 2015 19:35 | ||||||
| Last Modified: | 09 Mar 2020 13:18 |
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