Abstract
IT is more than a century since oriented fabrics were first noted in chondrites (see ref. 1), but since then little work has been done on the topic2,3, the most extensive being that by Dodd4. He found that most of his H- and L-group chondrites possessed foliation, together with lineation in the most strongly foliated specimens. The preferential orientation of elongated olivine phenocrysts in porphyritic chondrules has also been observed5.
This is a preview of subscription content, access via your institution
Access options
Subscribe to this journal
Receive 51 print issues and online access
$199.00 per year
only $3.90 per issue
Buy this article
- Purchase on Springer Link
- Instant access to full article PDF
Prices may be subject to local taxes which are calculated during checkout
Similar content being viewed by others
References
Wahl, W., Geochim. cosmochim. Acta, 2, 91 (1952).
Stacey, F. D., Lovering, J. F., and Parry, I., J. geophys. Res., 66, 1523 (1961).
Weaving, B., Geochim. cosmochim. Acta, 26, 451 (1962).
Dodd, R. T., Jr, Icarus, 4, 308 (1965).
Dodd, R. T., Jr, and Teleky, L. S., Icarus, 6, 407 (1967).
Whitaker, J. H. McD., and Gatrall, M., J. Geol., 77, 710 (1969).
Curray, J. R., J. Geol., 64, 117 (1956).
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
MARTIN, P., MILLS, A. & WALKER, E. Preferential orientation in four C3 chondritic meteorites. Nature 257, 37–38 (1975). https://doi.org/10.1038/257037a0
Received:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1038/257037a0
Comments
By submitting a comment you agree to abide by our Terms and Community Guidelines. If you find something abusive or that does not comply with our terms or guidelines please flag it as inappropriate.