High field magneto-transmission investigation of natural graphite
arXiv:1102.2756 · doi:10.1103/PhysRevB.83.073401
Abstract
Magneto-transmission measurements in magnetic fields in the range B=20-60T have been performed to probe the H and K-point Landau level transitions in natural graphite. At the H-point, two series of transitions, whose energy evolves as are observed. A reduced Slonczewski, Weiss and McClure (SWM) model with only two parameters to describe the intra-layer (gamma0) and inter-layer (gamma1) coupling correctly describes all observed transitions. Polarization resolved measurements confirm that the observed apparent splitting of the H-point transitions at high magnetic field cannot be attributed to an asymmetry of the Dirac cone.
5 pages, 3 figures
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Cited by in corpus (6)
- Using the de Haas-van Alphen effect to map out the closed three-dimensional Fermi surface of natural graphite
- Interaction-induced insulating state in thick multilayer graphene
- Decrypting the cyclotron effect in graphite using Kerr rotation spectroscopy
- Infrared magneto-spectroscopy of graphite in tilted fields
- Ultra-high magnetic field study of the layer split bands in Graphite
- Tight-binding description of Landau levels of graphite in tilted magnetic fields