Table T4.
Mineralogical assemblages of the clay fraction of sediments, Holes 1109B, 1109C, and 1109D.
interval (cm)
180-1109B-
1H-2, 145-150
2.9
xx
x
x
xx
xx
2H-3, 145-150
9.8
xx
x
x
xx
xx
2H-5, 145-150
12.1
xx
x
x
x
xx
xx
180-1109C-
3H-2, 145-150
19.9
xx
x
*
x
xx
5H-3, 145-150
40.4
xx
x (P)
x
xx
xx
6H-3, 145-150
49.9
xx
x (P)
x
xx
xx
8H-3, 145-150
68.9
xx
x (P)
*
xx
xx
10H-4, 115-120
89.1
xx
x
*
xx
xx
xx
xx
11H-3, 145-150
97.0
xx
x
*
*
xx
xx
xx
xx
14X-3, 145-150
126.1
xx
x
*
*
xx
xx
xx
xx
16X-3, 145-150
145.3
xx
x
*
xx
xx
xx
xx
18X-3, 115-120
164.3
xx
x
*
*
xx
xx
xxx
xx
23X-3, 33-43
212.4
xx
x
*
xx
xx
xx
xx
26X-1, 140-145
238.4
x
x
x
xx
xx
xx
xx
29X-3, 140-150
270.4
x
xx (P)
*
*
xx
xx
32X-3, 140-150
299.2
xx
x
*
xx
xxx
180-1109D-
35X-3, 140-150
328.3
xx
x
*
xxx
x
180-1109C-
39X-3, 140-150
357.0
x
x
xx
*
xxx
x
41X-2, 140-150
374.4
xx
x
*
xx
x
180-1109D-
7R-3, 120-130
410.7
xx
x
*
xx
x
9R-3, 101-111
430.1
xx
xx
x
xx
xx
11R-3, 122-132
449.3
xx
xx
*
xx
xx
13R-3, 79-89
467.9
xx
x
*
*
xxx
x
16R-5, 120-130
xx
x
*
*
xxx
18R-4, 120-130
517.7
xx
x
x
xx
x
22R-1, 124-134
552.4
*
*
xx
*
xx
x
26R-3, 30-40
583.0
xx
x
*
xxx
x
29R-2, 93-103
610.9
xx
xx (P)
x
*
xx
xx
34R-3, 123-133
661.0
x
*
*
xxx
x ?
38R-4, 150-150
701.4
xx
x
*
x
xxx
x
Notes: Assemblages were determined by X-ray diffraction analyses. C/S = chlorite-smectite mixed-layer, (P) = including feldspar. xxx = abundant, xx = common, x = rare, * = trace.
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