Shock wave studies in Blair dolomite
- 10 January 1980
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 85 (B1) , 293-297
- https://doi.org/10.1029/jb085ib01p00293
Abstract
Two types of shock wave experiments have been conducted on samples of Blair dolomite. The first employed a light‐gas gun to produce uniaxial strain, while the second used a spherical high‐explosive charge to cause radial divergent flow. Comparisons of data taken from these two types of experiments (at strain rates of 106/s and 104/s, respectively) with quasi‐static data (at 10−4/s) show that Blair dolomite is strongly time dependent in its behavior. This time dependence appears over the entire stress interval from 0.24 to 5.33 GPa.Keywords
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