Figure F46. Lower hemisphere equal-area stereographic projection of poles to brittle shear zones and fractures and the chrysotile foliation in Hole 1274A, measured in the core reference frame and rotated using the measured paleomagnetic declination back to a common orientation as described in "Structures in Peridotite and Gabbroic Intrusions," in "Mantle Upwelling, Melt Transport, and Igneous Crustal Accretion" in the "Leg 209 Summary" chapter.

Figure F46. Lower hemisphere equal-area stereographic projection of poles to brittle shear zones and fractures and the chrysotile foliation in Hole 1274A, measured in the core reference frame and rotated using the measured paleomagnetic declination back to a common orientation as described in "Structures in Peridotite and Gabbroic Intrusions" in "Mantle Upwelling, Melt Transport, and Igneous Crustal Accretion" in the "Leg 209 Summary" chapter.