Intercalation of bromine into single crystalline and well oriented pyrolytic graphite leads to the formation of several distinct, coexisting phases having compositions in the range C4600Br to C140Br. These phases are best regarded as graphitic regions of characteristic Fermi energy and dimensions, separated by condensed monolayers of Br- ions which have accepted their ionic charge from the pi electron system of the graphite matrix. Such acceptors do not markedly increase the collision broadening of the graphite Landau levels. Thus, using the transverse Shubnikov-de Haas effect, one can observe the dominant hole period which characterizes each phase of the graphite. Typically, the new hole periods are 5.27, 1.63, 1.24 and 0.21*10-6 G-1, which, using the Sloncewski-Weiss energy band model, give thicknesses for the individual tabular phases ranging from 700 to 21 AA, with corresponding Fermi energy depressions of 0.035 to 0.49 eV. In order of decreasing thickness, the Fermi surfaces of these phases evolve from the triple ellipsoids of pristine graphite through an elongated dumb-bell to an ovoid with a single extremum. The periods vary as the cosine of the angle of rotation of H away from c, confirming that in the present composition range the local ellipticity of the Fermi-surfaces remains of order 10. Landau state broadening and the relative stability of the new phases are briefly discussed.