Published August 2007
| Published
Journal Article
Open
Search for extinct ^(36)Cl in Ca-Al-rich inclusions in primitive ordinary chondrites
- Creators
-
Guan, Y.
- Ushikubo, T.
- Eiler, J. M.
- Kimura, M.
Abstract
The short-lived radionuclide ^(36)Cl decays to either ^(36)Ar (98.1%, β-) or ^(36)S (1.9%, ε and β+), with a half life of 3.01 × 10^5 yr [1]. Recent study has shown that ^(36)S anomalies from the decay of ^(36)Cl exist in sodalite (Na_8Al_6Si_6O_(24)Cl_2) of some Ningqiang CAIs and Allende CAIs and chondrule [2–5], but not in sodalite in other CAIs from Allende or Vigarano [6, 7]. In this study, we have expanded the search for ^(36)S anomalies in primitive ordinary chondrites.
Additional Information
© 2007 The Meteoritical Society.Attached Files
Published - Eiler_2007pA60.pdf
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Additional details
- Alternative title
- Search for extinct 36Cl in Ca-Al-rich inclusions in primitive ordinary chondrites
- Eprint ID
- 39559
- DOI
- 10.1111/j.1945-5100.2007.tb00601.x
- Resolver ID
- CaltechAUTHORS:20130724-135008010
- Created
-
2013-08-19Created from EPrint's datestamp field
- Updated
-
2021-11-09Created from EPrint's last_modified field
- Caltech groups
- Division of Geological and Planetary Sciences