Figure F67. Lower hemisphere stereographic projection of poles to crystal-plastic foliations, measured in the core reference frame and rotated into a common reference frame using the measured paleomagnetic declination as described in "Structures in Peridotite and Gabbroic Intrusions," in "Mantle Upwelling, Melt Transport, and Igneous Crustal Accretion" in the "Leg 209 Summary" chapter. All samples have measured negative inclinations, assumed to be indicative of a reversed polarity at the time of magnetization. The solid line connects measurements in Section 209-1270B-1R-1 (Piece 17) of a pyroxene band (Px) and a foliated oxide-microgabbro (mG) that crosscut a foliated coarse oxide gabbro (oxG).

Figure F67. Lower hemisphere stereographic projection of poles to crystal-plastic foliations, measured in the core reference frame and rotated into a common reference frame using the measured paleomagnetic declination as described in "Structures in Peridotite and Gabbroic Intrusions" in "Mantle Upwelling, Melt Transport, and Igneous Crustal Accretion" in the "Leg 209 Summary" chapter. All samples have measured negative inclinations, assumed to be indicative of a reversed polarity at the time of magnetization. The solid line connects measurements in Section 209-1270B-1R-1 (Piece 17) of a pyroxene band (Px) and a foliated oxide-microgabbro (mG) that crosscut a foliated coarse oxide gabbro (oxG).