Cosmic ray- and gas retention ages of newly recovered and of unusual chondrites

Citation
O. Eugster et al., Cosmic ray- and gas retention ages of newly recovered and of unusual chondrites, EARTH PLAN, 164(3-4), 1998, pp. 511-519
Citations number
29
Categorie Soggetti
Earth Sciences
Journal title
EARTH AND PLANETARY SCIENCE LETTERS
ISSN journal
0012821X → ACNP
Volume
164
Issue
3-4
Year of publication
1998
Pages
511 - 519
Database
ISI
SICI code
0012-821X(199812)164:3-4<511:CRAGRA>2.0.ZU;2-M
Abstract
We report the isotopic abundances of He, Ne, and Ar of four chondrites that fell in China, Jiange (H5), Juancheng (H5), Yanzhuang (H6), and Bo Xian (L L4), of Kagarlyk (L6) fallen in Russia, of Kress (L6) and Hunter (LL6) foun d in the USA, and of two Antarctic chondrites, Y-73001 (H4-6) and Y-73003 ( L5-6). The most important data that have direct consequences for the study of meteorite delivery dynamics to Earth crossing orbits are the cosmic ray exposure ages. They provide the constraints on meteorite origin, orbital ev olution, and regolith dynamics of the meteorite parent bodies. Dynamical st udies show how meteorites can reach Earth within a few million years. This time-scale can be checked against the cosmic ray exposure age determined fr om laboratory studies of the nuclides accumulated as a result of their expo sure to high energy particles. For Jiange, Juanchen, Yanzhuang, and Bo Xian we obtain cosmic ray exposure ages of 6.0, 5.3, 2.14, and 37.3 Ma, respect ively. Yanzhuang yields extremely low He-4 and Ar-40 gas retention ages and we conclude that this material experienced a thermal event at or before br eak-up of its parent body. Kagarlyk fell within five hours after the Tungus ka event in 1908 but we find that this meteorite is not related with the Tu nguska bolide. Kress yields an exposure age of 32 Ma whereas Hunter with 0. 5 Ma shows the shortest exposure age for any LL chondrite dated until now. The two Antarctic finds, Y-73001 and Y-73003 yield exposure ages of 16.1 Ma and 23.2 Ma, respectively. (C) 1998 Elsevier Science B.V. All rights reser ved.