
Figure F41. Lower hemisphere stereographic projection of poles to crystal-plastic foliations. A. Apparent dips as measured in the core face. B. Apparent dips 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. All samples have a normal polarity. All points are for protogranular shape fabrics in
harzburgite.

