Figure F67. Lower hemisphere stereoplots showing the orientation of poles to magmatic foliations, granophyric veins, and diabase contacts in Hole 1275B. A. Depth-sorted foliations. Circles = 50–140 mbsf, squares = 140–210 mbsf. B. Depth-sorted granophyre veins. Circles = 50–140 mbsf, squares = 140–210 mbsf. Measurements were rotated into a common orientation using the measured paleomagnetic azimuth as described in "Structures in Peridotite and Gabbroic Intrusions," in "Mantle Upwelling, Melt Transport, and Igneous Crustal Accretion" in the "Leg 209 Summary" chapter. It was assumed that samples from this hole record reversed polarity magnetization.

Figure F67. Lower hemisphere stereoplots showing the orientation of poles to magmatic foliations, granophyric veins, and diabase contacts in Hole 1275B. A. Depth-sorted foliations. Circles = 50–140 mbsf, squares = 140–210 mbsf. B. Depth-sorted granophyre veins. Circles = 50–140 mbsf, squares = 140–210 mbsf. Measurements were rotated into a common orientation using the measured paleomagnetic azimuth as described in "Structures in Peridotite and Gabbroic Intrusions," in "Mantle Upwelling, Melt Transport, and Igneous Crustal Accretion" in the "Leg 209 Summary" chapter. It was assumed that samples from this hole record reversed polarity magnetization.