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The magnetoresistance components and were measured in two p-Si/SiGe/Si quantum wells that have an anisotropic g-factor in a tilted magnetic field as a function of temperature, field and tilt angle. Activation energy measurements demonstrate the existence of a ferromagnetic-paramagnetic (F-P) transition for a sample with a hole density of =2,cm. This transition is due to crossing of the 0 and 1 Landau levels. However, in another sample, with =7.2,cm, the 0 and 1 Landau levels coincide for angles =0-70. Only for > 70 do the levels start to diverge which, in turn, results in the energy gap opening.

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