Meteorite shock stage is a measure of the degree of fracturing of the matrix of a common chondrite meteorite.[1] Impacts on the parent body of a meteoroid can produce very large pressures. These pressures heat, melt and deform the rocks. This is called shock metamorphism. Meteorites are often given a rating from 1 to 6 showing the level of shock metamorphism. However, the degree of shock can vary within a meteorite on the scale of centimeters.[2]
Smaller bodies colliding with one another would not have sufficiently great impact velocity to produce the pressures and temperatures required to produce shock effects, due to their lesser gravitational attraction for one another. High instantaneous pressures, in excess of 5 GPa (1 GPa = 10,000 atmospheres), are necessary to produce shock metamorphism.
- ^ "Some Fundamentals of Common Chondrite Classification". Archived from the original on 2016-06-12. Retrieved 2013-02-18.
- ^ Systematics and Evaluation of Meteorite Classification. Authors: Michael K. Weisberg, Timothy J. McCoy, Alexander N. Krot. PDF (page 32)