
Table
T10. Distribution
of volcanic components in core catcher samples from lithologic Units I, II, and
III at Hole 1138A.
Unit/Subunit |
Lithologies
with volcanic components |
Core,
section |
Depth
(mbsf) |
Feldspar |
Glass
(brown) |
Pumice |
Lithics |
Biotite |
Tephra
layer |
Age
(Ma) |
|
|
|
|
|
|
|
|
|
|
|
|
Foraminifer-bearing
diatom clay and
ooze |
1R-CC |
8.53 |
|
|
|
|
|
|
|
|
2R-CC |
12.78 |
|
|
|
|
|
|
|
|
|
3R-CC |
25.57 |
|
|
|
|
|
|
|
|
|
4R-CC |
34.94 |
|
|
|
|
|
|
|
|
|
5R-CC |
45.58 |
|
|
|
|
|
|
|
|
|
6R-CC |
49.65 |
|
|
|
|
|
|
|
|
|
7R-CC |
62.31 |
|
|
|
|
|
|
|
|
|
8R-CC |
74.04 |
|
|
|
|
|
|
|
|
|
9R-CC |
79.21 |
|
|
|
|
|
|
|
|
|
10R-CC |
87.53 |
|
|
|
|
|
|
|
|
|
11R-CC |
102.39 |
|
|
|
|
|
|
|
|
|
12R-CC |
107.03 |
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
Foraminifer-bearing
nannofossil clay |
13R-CC |
118.59 |
|
|
|
|
|
|
|
|
14R-CC |
126.23 |
|
|
|
|
|
|
|
|
|
15R-CC |
134.23 |
|
|
|
|
|
|
|
|
|
16R-CC |
145.85 |
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
Foraminifer-bearing
nannofossil
ooze |
17R-CC |
158.27 |
|
|
|
|
|
|
|
|
18R-CC |
168.84 |
|
|
|
|
|
|
|
|
|
19R-CC |
174.75 |
|
|
|
|
|
|
|
|
|
20R-CC |
186.14 |
|
|
|
|
|
|
|
|
|
21R-CC |
191.26 |
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
Foraminifer-bearing
nannofossil
chalk |
30R-CC |
278.21 |
|
|
|
|
|
|
|
|
31R-CC |
285.85 |
|
|
|
|
|
|
|
|
|
32R-CC |
296.3 |
|
|
|
|
|
|
|
|
|
33R-CC |
305.2 |
|
|
|
|
|
|
|
|
|
34R-CC |
319.09 |
|
|
|
|
|
|
|
|
|
35R-CC |
330.78 |
|
|
|
|
|
|
|
|
|
36R-CC |
340.6 |
|
|
|
|
|
|
|
|
|
37R-CC |
351.98 |
|
|
|
|
|
|
|
|
|
38R-CC |
357.21 |
|
|
|
|
|
|
|
|
|
39R-CC |
368.52 |
|
|
|
|
|
|
|
|
|
40R-CC |
375 |
|
|
|
|
|
|
|
|
|
41R-CC |
383.19 |
|
|
|
|
|
|
|
|
|
42R-CC |
397 |
|
|
|
|
|
|
|
Notes: Age determined from
"Biostratigraphy".
Volcanic components in >63 µm fraction of core catcher sample are
represented by A = abundant, C = common, P = present, and R = rare. Volcanic
components are not abundant in core catcher samples from 183-1138A-22R-CC
through 29R-CC and below 42R-CC in Subunit IIIA. Blank = not detected. T = a
discrete tephra layer was present in the core from which the core catcher was
examined. TT = two tephra layers were present.
