Abstract
The molecule exhibits a remarkable stability that leads to its survival in ancient carbonaceous rocks initially subjected to the elevated temperature requisite for its formation. Elementary particles having a large electronic stopping power can similarly form and higher fullerenes in their wake. Combined, these two features point at the possibility of using the presence in selected bulk geological samples as a new type of nuclear track detector, with applications in astroparticle physics.
- Received 15 March 1999
DOI:https://doi.org/10.1103/PhysRevLett.83.3097
©1999 American Physical Society