Core, section,
interval* (cm) |
Depth
(mcd) |
Chlorite
(%) |
Illite
(%) |
Kaolinite
(%) |
Smectite
(%) |
---|---|---|---|---|---|
184-1146B- | |||||
1H-1, 105 | 1.05 | 19.2 | 31.7 | 8.4 | 40.7 |
1H-2, 30 | 1.80 | 22.4 | 38.3 | 9.6 | 29.7 |
1H-2, 105 | 2.55 | 21.5 | 35.6 | 12.5 | 30.5 |
1H-3, 30 | 3.30 | 20.2 | 33.0 | 15.3 | 31.5 |
1H-3, 105 | 4.05 | 18.6 | 34.9 | 13.2 | 33.4 |
1H-4, 30 | 4.80 | 21.2 | 35.9 | 9.6 | 33.3 |
184-1146C- | |||||
1H-4, 105 | 6.45 | 21.9 | 37.6 | 9.6 | 30.9 |
1H-5, 30 | 7.20 | 25.7 | 37.4 | 12.6 | 24.3 |
1H-5, 105 | 7.95 | 24.9 | 41.2 | 8.7 | 25.3 |
1H-6, 30 | 8.70 | 31.2 | 42.6 | 2.1 | 24.2 |
1H-6, 105 | 9.45 | 19.7 | 35.1 | 9.9 | 35.3 |
184-1146B- | |||||
2H-2, 30 | 10.35 | 24.1 | 36.7 | 7.8 | 31.4 |
2H-2, 105 | 11.10 | 20.0 | 37.6 | 9.9 | 32.5 |
2H-3, 30 | 11.85 | 22.5 | 36.9 | 7.9 | 32.6 |
2H-3, 105 | 12.60 | 20.3 | 38.3 | 8.8 | 32.5 |
2H-4, 30 | 13.35 | 15.0 | 34.1 | 11.0 | 39.8 |
2H-4, 105 | 14.10 | 17.8 | 33.7 | 12.3 | 36.2 |
2H-5, 30 | 14.85 | 22.1 | 37.5 | 10.4 | 30.0 |
184-1146C- | |||||
2H-4, 30 | 15.90 | 20.3 | 38.8 | 9.6 | 31.4 |
2H-4, 105 | 16.65 | 17.8 | 37.1 | 11.7 | 33.4 |
2H-5, 30 | 17.40 | 14.8 | 38.5 | 11.2 | 35.5 |
2H-5, 105 | 18.15 | 18.2 | 36.7 | 9.7 | 35.4 |
2H-6, 30 | 18.90 | 9.4 | 31.4 | 11.3 | 48.0 |
2H-6, 105 | 19.65 | 19.8 | 36.1 | 10.5 | 33.6 |
2H-7, 30 | 20.40 | 20.3 | 39.5 | 11.1 | 29.2 |
184-1146B- | |||||
3H-2, 30 | 20.90 | 17.2 | 36.1 | 8.3 | 38.4 |
3H-2, 105 | 21.65 | 20.7 | 39.1 | 7.6 | 32.6 |
3H-3, 30 | 22.40 | 17.6 | 37.1 | 6.8 | 38.4 |
3H-3, 105 | 23.15 | 19.3 | 37.7 | 8.5 | 34.5 |
3H-4, 30 | 23.90 | 15.9 | 35.7 | 11.9 | 36.5 |
3H-5, 30 | 25.40 | 15.2 | 32.0 | 8.7 | 44.1 |
184-1146C- | |||||
3H-4, 30 | 25.60 | 17.9 | 36.4 | 11.5 | 34.1 |
3H-5, 30 | 27.10 | 19.7 | 35.0 | 14.5 | 30.8 |
3H-5, 105 | 27.85 | 20.1 | 33.7 | 14.2 | 32.1 |
3H-6, 30 | 28.60 | 22.5 | 36.5 | 12.1 | 28.9 |
184-1146B- | |||||
4H-1, 105 | 29.85 | 21.2 | 33.4 | 12.9 | 32.5 |
4H-2, 30 | 30.60 | 23.3 | 34.2 | 8.7 | 33.8 |
4H-2, 105 | 31.35 | 23.1 | 34.0 | 8.2 | 34.7 |
4H-3, 30 | 32.10 | 25.1 | 35.6 | 16.8 | 22.5 |
4H-3, 105 | 32.85 | 21.0 | 38.5 | 12.5 | 27.9 |
4H-4, 30 | 33.60 | 16.7 | 32.2 | 16.3 | 34.9 |
4H-4, 105 | 34.35 | 20.3 | 33.8 | 10.8 | 35.0 |
4H-5, 30 | 35.10 | 20.9 | 37.8 | 8.8 | 32.5 |
184-1146C- | |||||
4H-3, 105 | 36.00 | 19.8 | 37.8 | 12.2 | 30.2 |
4H-4, 30 | 36.75 | 22.6 | 34.9 | 10.0 | 32.5 |
4H-4, 105 | 37.50 | 22.0 | 39.5 | 10.3 | 28.1 |
4H-5, 30 | 38.25 | 25.0 | 37.7 | 8.8 | 28.5 |
4H-5, 105 | 39.00 | 24.7 | 36.6 | 9.7 | 29.0 |
184-1146B- | |||||
5H-1, 30 | 39.60 | 21.1 | 36.6 | 8.3 | 34.0 |
184-1146C- | |||||
4H-6, 30 | 39.75 | 22.5 | 38.2 | 7.4 | 31.8 |
184-1146B- | |||||
5H-2, 105 | 40.35 | 15.7 | 38.5 | 18.8 | 27.1 |
184-1146C- | |||||
4H-6, 105 | 40.50 | 25.5 | 37.4 | 5.4 | 31.7 |
184-1146B- | |||||
5H-2, 30 | 41.10 | 17.4 | 31.9 | 8.6 | 42.1 |
184-1146C- | |||||
4H-7, 30 | 41.25 | 21.7 | 36.1 | 10.2 | 32.0 |
5H-1, 30 | 41.50 | 18.0 | 30.5 | 8.1 | 43.4 |
184-1146B- | |||||
5H-2, 105 | 41.85 | 21.1 | 33.7 | 7.4 | 37.7 |
184-1146C- | |||||
5H-1, 105 | 42.25 | 19.2 | 34.4 | 11.1 | 35.2 |
5H-2, 30 | 43.00 | 20.1 | 35.8 | 10.1 | 34.0 |
5H-2, 105 | 43.75 | 21.3 | 36.9 | 9.6 | 32.3 |
184-1146B- | |||||
5H-4, 30 | 44.10 | 21.2 | 38.1 | 10.3 | 30.5 |
184-1146C- | |||||
5H-3, 30 | 44.50 | 12.0 | 30.1 | 10.7 | 47.1 |
184-1146B- | |||||
5H-4, 105 | 44.85 | 20.7 | 33.1 | 8.3 | 37.9 |
184-1146C- | |||||
5H-3, 105 | 45.25 | 20.4 | 36.3 | 8.7 | 34.6 |
184-1146B- | |||||
5H-5, 30 | 45.60 | 20.3 | 33.4 | 8.6 | 37.7 |
184-1146C- | |||||
5H-4, 30 | 46.00 | 16.3 | 33.3 | 12.5 | 37.9 |
184-1146B- | |||||
5H-5, 105 | 46.35 | 24.7 | 36.9 | 10.2 | 28.2 |
184-1146C- | |||||
5H-4, 105 | 46.75 | 21.3 | 34.8 | 13.1 | 30.9 |
184-1146C- | |||||
5H-6, 30 | 47.10 | 20.0 | 34.0 | 13.5 | 32.5 |
184-1146C- | |||||
5H-5, 30 | 47.50 | 20.1 | 35.0 | 12.9 | 32.0 |
5H-5, 105 | 48.25 | 25.2 | 32.4 | 6.8 | 35.5 |
5H-6, 30 | 49.00 | 21.2 | 33.8 | 9.1 | 36.0 |
184-1146B- | |||||
6H-1, 105 | 49.75 | 26.3 | 40.2 | 12.1 | 21.3 |
6H-2, 30 | 50.50 | 24.8 | 37.7 | 15.6 | 21.9 |
6H-2, 105 | 51.25 | 25.3 | 35.8 | 10.1 | 28.9 |
6H-3, 30 | 52.00 | 21.4 | 36.3 | 11.7 | 30.7 |
6H-3, 105 | 52.75 | 21.5 | 34.9 | 7.6 | 36.0 |
6H-4, 30 | 53.50 | 25.3 | 35.0 | 7.6 | 32.1 |
6H-4, 105 | 54.25 | 19.7 | 36.9 | 8.4 | 35.0 |
6H-5, 30 | 55.00 | 23.7 | 40.2 | 10.0 | 26.1 |
6H-5, 105 | 55.75 | 20.9 | 35.3 | 9.6 | 34.2 |
6H-6, 30 | 56.50 | 24.3 | 34.7 | 6.8 | 34.3 |
6H-6, 105 | 57.25 | 22.0 | 36.6 | 8.2 | 33.2 |
184-1146C- | |||||
6H-5, 30 | 57.65 | 24.1 | 36.6 | 7.2 | 32.0 |
6H-5, 105 | 58.40 | 21.7 | 26.5 | 4.9 | 46.9 |
6H-6, 30 | 59.15 | 21.0 | 33.3 | 9.0 | 36.8 |
6H-6, 105 | 59.90 | 19.9 | 28.7 | 9.3 | 42.1 |
184-1146B- | |||||
7H-2, 30 | 60.60 | 18.8 | 33.7 | 13.3 | 34.2 |
7H-2, 105 | 61.35 | 19.3 | 32.0 | 11.4 | 37.3 |
7H-3, 30 | 62.10 | 21.9 | 27.7 | 9.5 | 40.9 |
7H-3, 105 | 62.85 | 24.5 | 31.6 | 8.6 | 35.4 |
7H-4, 30 | 63.60 | 18.8 | 34.2 | 11.8 | 35.2 |
Notes: Clay mineral content corresponds to semiquantitative data, based on the measurement of the surface of the basal reflection on the ethylene glycol XRD diagram. Smectite content combines smectite and illite-smectite mixed-layer minerals. * = all intervals are 2 cm long, and the top of each interval is given. Only a portion of this table appears here. The complete table is available in ASCII.