Contributions to Mineralogy and Petrology

, Volume 58, Issue 1, pp 37–49

Variations in shock deformation at the Slate Islands impact structure, Lake Superior, Canada

  • Richard A. F. Grieve
  • P. Blyth Robertson
Article

DOI: 10.1007/BF00384743

Cite this article as:
Grieve, R.A.F. & Robertson, P.B. Contr. Mineral. and Petrol. (1976) 58: 37. doi:10.1007/BF00384743

Abstract

A progressive change in the level of shock deformation is documented in autochthonous rocks from the central uplift of the Slate Islands impact structure, Lake Superior. Correlation of these observations, which are based mainly on the relative frequency of planar features of specific crystallographic orientation in quartz, with experimental data is used to estimate the average shock pressures recorded in the samples studied. Recorded pressures range from 5.8 to 15.3 GPa and generally increase towards the proposed shock centre. Variations in the shock response of quartz of different grain size and texture are observed within and between samples. It is apparent that large interlocking quartz grains in “eyes” record approximately 15–20% higher levels of shock deformation than small grains in mosaics or large isolated phenocrysts. These variations in shock deformation are attributed to the effect of shock wave reverberations between grains and length of shock pulse duration within grains.

Comparison of the Slate Islands data with similar observations at the larger Charlevoix impact structure indicates that the rate of change of recorded shock pressure with distance is greater at the Slate Islands structure. This is interpreted as due to variations in the strain rates and/or the rate of shock wave attenuation with radial distance between impact structures of different size.

Copyright information

© Springer-Verlag 1976

Authors and Affiliations

  • Richard A. F. Grieve
    • 1
  • P. Blyth Robertson
    • 1
  1. 1.Department of Energy, Mines and ResourcesGravity and Geodynamics Division, Earth Physics BranchOttawaCanada