“…A special form of parting is composed of altered volcanic ash layers (tornstein) which represent volcanic events of short duration and therefore are nearly isochronous horizons, such as in the Ferron group in Utah, which may also be found within coal seams (Lamarre, 2003). Rock partings or parting layers create density variations in the coal, which are a function of mineral material, or ash, within the coal seam (Beaton et al, 2006;Manchioni, 2003). Most importantly in relation to fluid and gas flow, these partings create strong discontinuities in the petrophysical fabric (porosity and permeability) within the coalbed methane reservoir.…”