Abstract
The Fermi surface of graphite has been mapped out using de Haas–van Alphen (dHvA) measurements at low temperature with in-situ rotation. For tilt angles between the magnetic field and the axis, the majority electron and hole dHvA periods no longer follow a behavior demonstrating that graphite has a three-dimensional closed Fermi surface. The Fermi surface of graphite is accurately described by highly elongated ellipsoids. A comparison with the calculated Fermi surface suggests that the Slonczewski-Weiss-McClure trigonal warping parameter is significantly larger than previously thought.
- Received 10 November 2011
DOI:https://doi.org/10.1103/PhysRevLett.108.117401
© 2012 American Physical Society