Figure F14. Bulk powder X-ray diffractograms of samples from selected intervals in Hole U1322B. All diffractograms have the same vertical scale. Thin vertical lines denote characteristic mineral peaks: I/M = illite/mica, K + C = kaolinite + chlorite, M = mica, Ph = phyllosilicates, Qz = quartz, kF = potassium feldspar, Pl = plagioclase, Ca = calcite, Do = dolomite, Ha = halite.
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