Figure F46. Lower hemisphere equal-area stereographic projection of poles to black-dark green serpentine and white- and green-banded serpentine veins in Hole 1272A, 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 black-dark green serpentine and white- and green-banded serpentine veins in Hole 1272A, 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.