Impact Breccias in the Central Vredefort Dome -- Revisited
Abstract
Vredefort Dome pseudotachylites have a random, Granophyre a radial orientation, independent from target rock structures. Pseudotachylites form through explosive transfer of thermal shock energy. Boulders similar to Sudbury Footwall Breccia occur.
- Publication:
-
Lunar and Planetary Science Conference
- Pub Date:
- March 2003
- Bibcode:
- 2003LPI....34.1019D