Abstract
BERWERTH1 reported monoclinic pyroxene (diopside), orthopyroxene, glass, and a sodium–iron–aluminium silicate, weinbergerite, in the octahedrite iron, Kodaikanal. So far, however, all his observations have not been verified. In fact, diopside (or pigeonite) is considered to occur only in some achondrites, chondrites, and mesosiderites2. Glass of intermediate plagioclase composition (maskelynite) is found in several chondrites2; however, Marvin3 reported a relatively high-index glass (n= 1.60) in the iron, Carbo.
Similar content being viewed by others
References
Berwerth, F., Tscher. Mineral, und Petrol. Mitt., 25, 179 (1906).
Mason, B., Meteorites (Wiley, New York, 1962).
Marvin, U., Nature, 196, 634 (1962).
Krinov, E., Principles of Meteoritics (Pergamon, London, 1961).
Prior, G., Catalogue of Meteorites (British Museum (Nat. Hist.), second ed., 1953).
Lipschutz, M., and Anders, E., Geochim. et Cosmochim. Acta, 24, 83 (1961).
Roedder, E., Amer. Mineral., 36, 282 (1951).
Holgate, N., J. Geol., 62, 439 (1954).
Work carried out by P. Moore, Department of Geophysical Sciences, University of Chicago.
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
OLSEN, E., MUELLER, R. Silicates in some Iron Meteorites. Nature 201, 596–597 (1964). https://doi.org/10.1038/201596a0
Issue Date:
DOI: https://doi.org/10.1038/201596a0
- Springer Nature Limited
This article is cited by
-
Concordant 3,676 Myr U–Pb formation age for the Kodaikanal iron meteorite
Nature (1985)
-
Mineralogy and petrology of silicate inclusions in iron meteorites
Contributions to Mineralogy and Petrology (1970)