Published July 2012
| Published
Journal Article
Open
Oxygen Isotopes of Al-Rich Chondrules from Unequilibrated Ordinary Chondrites
Abstract
Al-rich chondrules (ARCs) are a rare constituent of chondrites. They have relatively high bulk Al_2O_3 content (> 10 wt%), which is due to the presence of Al-rich phases, such as plagioclase, spinel, Al-rich glass etc. [1]. ARCs share some chemical and petrologic characteristics with Ca, Al-rich inclusions (CAis), and may represent a genetic link between ferromagnesian chondrules and CAis.
Additional Information
© 2012 Meteoritical Society. Issue published online: 6 Aug 2012. Article first published online: 8 Aug 2012. Samples used in this study are provided by the Polar Research Institute of China. This work was supported by the National NSF of China (Grant No. 41173076 and 10921063) and by the Minor Planet Foundation of China.Attached Files
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Additional details
- Eprint ID
- 34644
- DOI
- 10.1111/j.1945-5100.2012.01401_2.x
- Resolver ID
- CaltechAUTHORS:20121002-152731528
- 41173076
- National Natural Science Foundation of China
- 10921063
- National Natural Science Foundation of China
- Minor Planet Foundation of China
- Created
-
2012-10-02Created from EPrint's datestamp field
- Updated
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2021-11-09Created from EPrint's last_modified field