Core, section, interval (cm)
|
Depth (mbsf)
|
Piece
|
Lithology
|
N
|
Decay type
|
MAD (°)
|
Remanence direction (°)
|
Demagnetization (mT)
|
J
(A/m) |
PCA
(%) |
||
---|---|---|---|---|---|---|---|---|---|---|---|---|
Declination
|
Inclination
|
Low
|
High
|
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209-1271A- |
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1R-1, 44 | 0.44 | 9 | 1 | 5 | F | 2.8 | 252.5 | 14.6 | 15 | 40 | 0.2107 | 7.8 |
1R-1, 60 | 0.60 | 10 | 1 | 4 | F | 2.7 | 91.2 | 34.0 | 20 | 40 | 0.8205 | 6.4 |
1R-1, 78 | 0.78 | 11 | 1 | 3 | A | 2.2 | 51.6 | 35.9 | 25 | 40 | 1.0494 | 6.2 |
1R-1, 98 | 0.98 | 12 | 1 | 3 | A | 2.3 | 37.0 | 34.6 | 25 | 40 | 0.9933 | 6.7 |
1R-1, 114 | 1.14 | 14 | 1 | 3 | A | 1.0 | 41.3 | 24.5 | 25 | 40 | 0.7309 | 14.2 |
1R-2, 32 | 1.74 | 7 | 1 | 3 | A | 2.0 | 79.5 | 23.6 | 25 | 40 | 0.2849 | 60.1* |
1R-2, 70 | 2.12 | 14 | 1 | 3 | A | 0.8 | 179.3 | 29.6 | 25 | 40 | 0.133 | 60.1* |
1R-2, 90 | 2.32 | 18 | 1 | 3 | A | 1.3 | 267.5 | 24.1 | 25 | 40 | 0.149 | 57.8* |
1R-2, 106 | 2.48 | 19 | 1 | 2 | A | 2.2 | 252.6 | 31.5 | 30 | 40 | 0.2649 | 41.4* |
3R-1, 64 | 19.54 | 11 | 1 | 2 | A | 2.9 | 33.0 | 56.8 | 30 | 40 | 0.0905 | 2.4 |
4R-1, 22 | 28.72 | 5 | 17 | 5 | F | 1.7 | 78.6 | 8.4 | 15 | 40 | 0.4551 | 9.2 |
4R-1, 82 | 29.32 | 13 | 17 | 4 | F | 2.8 | 34.7 | 27.2 | 20 | 40 | 0.2888 | 3.3 |
4R-1, 94 | 29.44 | 14 | 17 | 3 | F | 3.9 | 222.0 | 29.0 | 25 | 40 | 0.1687 | 2.0 |
4R-1, 110 | 29.60 | 17 | 17 | 2 | A | 3.1 | 91.3 | 24.8 | 30 | 40 | 0.1329 | 1.9 |
4R-2, 6 | 29.83 | 1 | 17 | 4 | F | 1.2 | 32.4 | 36.7 | 20 | 40 | 0.1932 | 2.2 |
4R-2, 42 | 30.19 | 2 | 17 | 4 | F | 1.8 | 12.2 | 7.3 | 20 | 40 | 0.4682 | 6.4 |
4R-2, 52 | 30.29 | 3 | 17 | 4 | F | 2.3 | 165.9 | 39.0 | 20 | 40 | 0.2213 | 3.1 |
4R-2, 56 | 30.33 | 3 | 17 | 4 | F | 2.4 | 183.9 | 22.5 | 20 | 40 | 0.3374 | 3.9 |
4R-2, 68 | 30.45 | 4 | 17 | 4 | F | 0.8 | 206.7 | 13.7 | 20 | 40 | 0.2786 | 4.7 |
4R-2, 84 | 30.61 | 6 | 17 | 4 | F | 1.7 | 301.4 | 22.1 | 20 | 40 | 0.4467 | 6.4 |
4R-2, 110 | 30.87 | 7 | 17 | 3 | A | 3.1 | 237.5 | 9.5 | 25 | 40 | 0.3796 | 5.2 |
209-1271B- |
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|
|
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5R-1, 52 | 28.22 | 10 | 1 | 2 | A | 0.4 | 169.0 | 16.0 | 40 | 50 | 0.335 | 9.7 |
7R-1, 20 | 36.40 | 4 | 1 | 5 | A | 2.0 | 130.4 | 36.8 | 20 | 50 | 0.1589 | 3.6 |
7R-1, 28 | 36.48 | 5 | 1 | 4 | F | 3.1 | 45.3 | 33.1 | 25 | 50 | 0.1273 | 2.6 |
7R-1, 54 | 36.74 | 7 | 1 | 4 | F | 1.0 | 41.4 | 22.9 | 25 | 50 | 0.257 | 11.5 |
8R-1, 74 | 41.44 | 14 | 1 | 4 | F | 4.3 | 53.3 | 34.8 | 25 | 50 | 0.2861 | 2.5 |
10R-1, 110 | 51.60 | 19 | 2 | 4 | F | 3.2 | 311.2 | 14.3 | 25 | 50 | 0.6778 | 9.2 |
10R-1, 124 | 51.74 | 20 | 2 | 4 | F | 3.6 | 50.3 | 27.7 | 25 | 50 | 0.192 | 8.2 |
11R-1, 104 | 56.54 | 19 | 1 | 4 | F | 2.8 | 268.6 | 28.8 | 25 | 50 | 0.7036 | 15.9 |
11R-1, 114 | 56.64 | 20 | 1 | 4 | F | 2.6 | 239.2 | 24.9 | 25 | 50 | 1.4958 | 25.3 |
12R-1, 38 | 60.48 | 7 | 14 | 4 | F | 2.2 | 23.8 | 24.7 | 25 | 50 | 0.666 | 18.0 |
12R-1, 52 | 60.62 | 8 | 14 | 4 | F | 2.4 | 128.9 | –28.7 | 25 | 50 | 1.0623 | 22.4† |
12R-1, 74 | 60.84 | 12 | 14 | 4 | F | 3.4 | 252.0 | 45.9 | 25 | 50 | 0.6995 | 15.0 |
12R-1, 98 | 61.08 | 16 | 14 | 4 | F | 0.9 | 322.5 | 18.5 | 25 | 50 | 0.4563 | 17.4 |
12R-1, 134 | 61.44 | 21 | 14 | 4 | F | 2.3 | 269.7 | 35.7 | 25 | 50 | 1.252 | 15.9 |
13R-1, 56 | 65.66 | 10 | 1 | 4 | F | 2.3 | 185.1 | 36.8 | 25 | 50 | 0.0705 | 5.2 |
14R-1, 18 | 69.98 | 4 | 10 | 3 | A | 2.4 | 254.5 | 21.7 | 25 | 40 | 0.0001 | 31.1 |
15R-1, 26 | 75.06 | 5 | 1 | 4 | A | 1.2 | 146.9 | 28.4 | 25 | 50 | 0.4069 | 15.6 |
17R-1, 12 | 84.62 | 2 | 10 | 4 | F | 6.4 | 98.4 | 23.5 | 25 | 50 | 0.0002 | 37.1 |
17R-1, 62 | 85.12 | 10 | 1 | 3 | F | 2.4 | 182.6 | 57.2 | 30 | 50 | 0.0727 | 1.6 |
17R-1, 104 | 85.54 | 16 | 2 | 5 | F | 1.5 | 356.8 | 27.5 | 20 | 50 | 0.8441 | 9.4 |
18R-1, 54 | 89.64 | 10 | 1 | 5 | F | 1.8 | 161.3 | 8.5 | 20 | 50 | 0.5953 | 17.1 |
18R-1, 112 | 90.22 | 20 | 1 | 5 | F | 0.9 | 325.5 | 25.7 | 20 | 50 | 0.5114 | 29.2 |
19R-1, 16 | 94.26 | 3 | 1 | 5 | F | 1.3 | 10.8 | 37.2 | 20 | 50 | 0.3452 | 3.7 |
19R-2, 8 | 95.68 | 1 | 1 | 5 | F | 2.3 | 324.6 | 52.2 | 20 | 50 | 0.4363 | 3.9 |
20R-1, 84 | 99.64 | 16 | 1 | 4 | F | 2.5 | 359.7 | 37.6 | 20 | 40 | 0.13 | 3.7 |
Notes: Lithology: 1 = dunite, 2 = harzburgite, 10 = gabbro, 14 = troctolite, 17 = serpentinite. N = number of samples. Decay type: A = anchored to origin, F = free of origin. MAD = maximum angular deviation. PCA (%) = percentage of natural remanent magnetization intensity. * = PCA (%) normalized to 15-mT demagnetization step. † = sample marked upside down. Corrected direction = 231/28.7. This table is also available in ASCII.