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Table T23. Mean paleomagnetic direction for each core, Site U1332. (See table notes.)
|
Core
|
Inclination
(°)
|
Declination
(°)
|
N
|
α95
(°)
|
|
320-U1332A-
|
|
1H
|
–6.6
|
352.1
|
47
|
4.4
|
|
2H
|
–76.1
|
28.0
|
170
|
8.4
|
|
3H
|
3.4
|
156.3
|
162
|
4.7
|
|
4H
|
3.7
|
86.7
|
174
|
3.0
|
|
5H
|
–4.7
|
345.9
|
177
|
2.6
|
|
6H
|
7.6
|
192.5
|
164
|
2.1
|
|
7H
|
–2.3
|
261.1
|
175
|
4.0
|
|
8H
|
8.6
|
162.3
|
171
|
2.9
|
|
9H
|
3.3
|
104.5
|
176
|
1.4
|
|
10H
|
4.9
|
121.5
|
162
|
1.5
|
|
11H
|
5.7
|
263.3
|
132
|
2.0
|
|
12H
|
3.2
|
293.1
|
143
|
1.5
|
|
13H
|
–14.8
|
279.0
|
175
|
2.2
|
|
14H
|
–11.6
|
99.0
|
118
|
2.2
|
|
320-U1332B-
|
|
1H
|
6.9
|
340.9
|
32
|
4.4
|
|
2H
|
30.0
|
101.8
|
170
|
6.9
|
|
3H
|
5.9
|
68.1
|
107
|
4.0
|
|
4H
|
6.0
|
68.6
|
147
|
3.0
|
|
5H
|
12.4
|
219.9
|
127
|
3.0
|
|
6H
|
13.6
|
194.1
|
114
|
3.2
|
|
7H
|
–5.9
|
105.0
|
174
|
2.9
|
|
8H
|
7.9
|
188.8
|
132
|
2.8
|
|
9H
|
3.6
|
120.6
|
170
|
1.8
|
|
10H
|
7.4
|
57.9
|
148
|
2.8
|
|
11H
|
4.6
|
18.7
|
99
|
3.8
|
|
12H
|
10.4
|
238.2
|
156
|
2.4
|
|
13H
|
–3.2
|
152.1
|
161
|
1.8
|
|
320-U1332C-
|
|
1H
|
21.9
|
142.9
|
151
|
15.6
|
|
2H
|
17.4
|
5.8
|
151
|
5.0
|
|
3H
|
–1.7
|
125.7
|
145
|
3.6
|
|
4H
|
9.1
|
179.8
|
172
|
2.7
|
|
5H
|
3.5
|
215.4
|
169
|
1.4
|
|
6H
|
5.4
|
240.2
|
85
|
2.2
|
|
7H
|
–0.1
|
335.5
|
172
|
2.5
|
|
8H
|
5.8
|
120.6
|
134
|
2.5
|
|
9H
|
6.4
|
219.8
|
165
|
2.4
|
|
11H
|
2.2
|
82.4
|
148
|
1.4
|
|
12H
|
3.0
|
92.8
|
155
|
1.4
|
|
13H
|
–8.4
|
25.2
|
148
|
2.0
|
Notes: Mean paleomagnetic directions and statistics calculated using Bingham statistics for each core. Inclination = mean paleomagnetic inclination from stable polarity intervals in core, declination = mean paleomagnetic declination from stable polarity intervals in core. By subtracting this value from observed paleomagnetic declinations measured along core, core can be approximately reoriented back into geographic coordinates. After reorientation, normal polarity intervals will have ~0° declination and reversed polarity intervals will have ~180° declination. N = number of paleomagnetic observations used in calculating mean, α95 = 95% confidence angle for mean direction.
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