Figure F2. Close-up photographs. A, B. High-angle normal faults in Unit I. In both examples, the fault (the surface of which is outlined by concentration of black pyrite) offsets lighter nannofossil layers. C. Yellow coarse-grained foraminifer-bearing intervals associated with pyrite-rich layers in Subunit IA. D. Brown bioturbated nannofossil ooze layer interbedded with a green diatom ooze. E. High-angle lamination, most likely a result of soft-sediment deformation in Subunit IA. F. Oblique fissility in Subunit ID. G. Pervasive scaly fabric in Unit II. H. Brecciated dolomite layer in Unit II. I. Carbonate nodules from Subunit II.

Figure F2. Close-up photographs. A, B. High-angle normal faults in Unit I. In both examples, the fault (the surface of which is outlined by concentration of black pyrite) offsets lighter nannofossil layers. C. Yellow coarse-grained foraminifer-bearing intervals associated with pyrite-rich layers in Subunit IA. D. Brown bioturbated nannofossil ooze layer interbedded with a green diatom ooze. E. High-angle lamination, most likely a result of soft-sediment deformation in Subunit IA. F. Oblique fissility in Subunit ID. G. Pervasive scaly fabric in Unit II. H. Brecciated dolomite layer in Unit II. I. Carbonate nodules from Subunit II.