Meteoritics & Planetary Science, Volume 39, Number 10 (2004)http://hdl.handle.net/10150/6412812024-03-28T18:05:44Z2024-03-28T18:05:44ZEditorialSears, Derek W. G.http://hdl.handle.net/10150/6566792021-02-16T01:53:38Z2004-01-01T00:00:00ZEditorial
Sears, Derek W. G.
2004-01-01T00:00:00ZBook Review: A Visitor's Guide to the Kitt Peak Observatories, Leslie Sage, Gail AschenbrennerBrocious, D.http://hdl.handle.net/10150/6559192021-02-14T01:17:57Z2004-01-01T00:00:00ZBook Review: A Visitor's Guide to the Kitt Peak Observatories, Leslie Sage, Gail Aschenbrenner
Brocious, D.
Book Review: A Visitor's Guide to the Kitt Peak Observatories, Leslie Sage, Gail Aschenbrenner. Cambridge University Press (2004).
2004-01-01T00:00:00ZThe new Arthur Ross Hall of Meteorites at the American Museum of Natural HistoryEbel, D. S.Boesenberg, J. S.http://hdl.handle.net/10150/6559182021-02-14T01:17:24Z2004-01-01T00:00:00ZThe new Arthur Ross Hall of Meteorites at the American Museum of Natural History
Ebel, D. S.; Boesenberg, J. S.
2004-01-01T00:00:00ZAnomalous Mössbauer parameters in the second generation regolith Ghubara meteoriteVerma, H. C.Tripathi, R. P.http://hdl.handle.net/10150/6559172021-02-14T01:16:59Z2004-01-01T00:00:00ZAnomalous Mössbauer parameters in the second generation regolith Ghubara meteorite
Verma, H. C.; Tripathi, R. P.
We conducted Mössbauer spectroscopic studies on the Ghubara meteorite which had been described as at least two-generation regolith breccia on the macro scale. The isomer shift and quadrupole splitting of the Fe-Ni part are quite different from those obtained in ordinary chondrites, reflecting shock effects. We observed a large amount of magnetite that may have come from weathering of, primarily, the silicate fraction. We found very similar iron mineralogy in the Densmore meteorite.
2004-01-01T00:00:00Z