Abstract
Anomalous shocked quartz with high density (less than 1 % of density-deviation) is considered to be a relict of ultra high-pressure at meteoritic impact. The shocked quartz grains can be found only in terrestrial and artificial impact craters, meteorites and the Cretaceous-Tertiary (K/T) boundary samples. Volcanic activity is considered to be started or accelerated by enormous impact event.
Similar content being viewed by others
References
Alvarez, L.W., Alvarez, W., Asaro, F. and Michel, H.V.: 1980, Science 208, 1095–1108
Bohor, B.F., Modreski, P.J. and Foord, E.E.: 1987, Science 236, 705–709
Kyte, F.T., Zhou, Z. and Wasson, J.T.: 1980, Nature 288, 651–656
McHone, J.F., Niema, R.A., Lewis, C.F. and Yates, A.M.: 1989, Science 243, 776–779
Miura, Y.: 1991a, Shock Waves 1, 35–41
Miura, Y.: 1991b, Lunar and Planetary Science XXII, (LPI, Houston), 905–908
Miura, Y. and Kato, T.: 1991, Symp. Antartic Meteorites, NIPR, Tokyo, 18, 17–19
Montanari, A., Hay, R.L., Alvarez, W., Asaro, F., Michel, H.V., Alvarez L. and Smit, J.: 1983, Geology 11, 668–671
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
MIURA, Y., KATO, T. & Imai, M. Evidence of earth catastrophe by anomalous shocked quartz at the K/T boundary. Celestial Mech Dyn Astr 54, 249–253 (1992). https://doi.org/10.1007/BF00049559
Issue Date:
DOI: https://doi.org/10.1007/BF00049559