Abstract
We discuss the known experimental data on the phase of the de Haas–van Alphen oscillations in graphite. These data can be understood if one takes into account that four band-contact lines exist near the HKH edge of the Brillouin zone of graphite.
- Received 1 February 2006
DOI:https://doi.org/10.1103/PhysRevB.73.235112
©2006 American Physical Society