Figure F72. Downhole variation in natural remanent magnetization (NRM) intensity, magnetic susceptibility, Koenigsberger ratio (Q-ratio), and percentage of NRM removed by 20-mT alternating-field demagnetization for the volcaniclastic subunits in Hole 1184A. See "Rock-Magnetic Properties" in "Paleomagnetism" for discussion. See legend in Figure F10.