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A series of 140 samples from Holes 417A, 417B, 418A, and 418B were examined semiquantitatively for their X-ray mineralogy. We selected most samples from the dominant lithologies rather than by coring the same sedimentary sequence at Sites 417 and 418, only 8 km apart (Figure 1). Both sites are located at the foot of the Bermuda Rise (Figure 2) along the MO magnetic anomaly on crust of lower Aptian age. Sediments are mainly abyssal pelagic clays, with various authigenic minerals low in carbonates.

X-Ray Mineralogy of Deep Sea Drilling Project Legs 51 through 53, Western North Atlantic