van Andel, Tjeerd H; Heath, G Ross (2004): Mineral composition of clay fraction from Hole 16-162 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.219759
Always quote citation above when using data! You can download the citation in several formats below.
Related to:
DSDP (1989): Data from the Deep Sea Drilling Project. Sediment, hard rock and reference files. National Geophysical Data Center, National Environmental Satellite, Data and Information Service, National Oceanic and Atmospheric Administration, U.S. Department of Commerce, 1, CD-ROM
Yeats, Robert S; Rodolfo, Kelvin S; Kaneps, Ansis G; Dinkelman, Menno G; Cronan, David S; Charleston, Santiago; Bukry, David; Bennett, Richard H; van Andel, Tjeerd H; Heath, G Ross (1973): Initial Reports of the Deep Sea Drilling Project 16. Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, XVI, 949 pp, https://doi.org/10.2973/dsdp.proc.16.1973
Further details:
X-ray mineralogy data base - Background and methods. hdl:10013/epic.32358.d001
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: 14.869800 * Longitude: -140.043500
Date/Time Start: 1971-03-15T00:00:00 * Date/Time End: 1971-03-15T00:00:00
Minimum DEPTH, sediment/rock: 0.405 m * Maximum DEPTH, sediment/rock: 146.950 m
Event(s):
16-162 * Latitude: 14.869800 * Longitude: -140.043500 * Date/Time: 1971-03-15T00:00:00 * Elevation: -4854.0 m * Penetration: 153 m * Recovery: 130.8 m * Location: North Pacific/CONT RISE * Campaign: Leg16 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 17 cores; 153 m cored; 0 m drilled; 85.5 % recovery
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
2 | Sample code/label | Sample label | DSDP/ODP/IODP sample designation | |||
3 | Depth, top/min | Depth top | m | |||
4 | Depth, bottom/max | Depth bot | m | |||
5 | Clinoptilolite | Cpt | % | X-ray diffraction, clay fraction | ||
6 | Gypsum | Gp | % | X-ray diffraction, clay fraction | ||
7 | Halite | Hl | % | X-ray diffraction, clay fraction | ||
8 | Kaolinite | Kln | % | X-ray diffraction, clay fraction | ||
9 | Mica | Mica | % | X-ray diffraction, clay fraction | ||
10 | Montmorillonite | Mnt | % | X-ray diffraction, clay fraction | ||
11 | Phillipsite | Php | % | X-ray diffraction, clay fraction | ||
12 | Plagioclase | Pl | % | X-ray diffraction, clay fraction | ||
13 | Quartz | Qz | % | X-ray diffraction, clay fraction |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
158 data points
Data
1 Depth sed [m] | 2 Sample label | 3 Depth top [m] | 4 Depth bot [m] | 5 Cpt [%] | 6 Gp [%] | 7 Hl [%] | 8 Kln [%] | 9 Mica [%] | 10 Mnt [%] | 11 Php [%] | 12 Pl [%] | 13 Qz [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|
0.405 | 16-162-1 | 0.0 | 0.81 | 12.3 | 46.3 | 28.4 | 13.0 | |||||
2.705 | 16-162-1 | 0.0 | 5.41 | 16.5 | 37.7 | 30.5 | 15.2 | |||||
3.755 | 16-162-1 | 0.0 | 7.51 | 70.0 | 13.0 | 11.1 | 5.9 | |||||
12.770 | 16-162-2 | 9.0 | 16.54 | 4.7 | 18.5 | 39.5 | 16.8 | 8.4 | 12.1 | |||
21.770 | 16-162-3 | 18.0 | 25.54 | 74.0 | 11.0 | 10.4 | 4.5 | |||||
29.265 | 16-162-4 | 27.0 | 31.53 | 79.2 | 14.7 | 6.0 | ||||||
37.205 | 16-162-5 | 36.0 | 38.41 | 80.8 | 13.3 | 5.9 | ||||||
39.770 | 16-162-5 | 36.0 | 43.54 | 11.7 | 74.6 | 9.9 | 3.7 | |||||
47.270 | 16-162-6 | 45.0 | 49.54 | 1.1 | 89.6 | 6.6 | 2.7 | |||||
55.955 | 16-162-7 | 54.0 | 57.91 | 89.4 | 7.2 | 3.2 | ||||||
57.770 | 16-162-7 | 54.0 | 61.54 | 84.0 | 9.6 | 6.4 | ||||||
66.770 | 16-162-8 | 63.0 | 70.54 | 50.3 | 9.9 | 28.3 | 11.5 | |||||
75.770 | 16-162-9 | 72.0 | 79.54 | 93.4 | 5.2 | 1.4 | ||||||
83.270 | 16-162-10 | 81.0 | 85.54 | 2.6 | 97.5 | |||||||
93.015 | 16-162-11 | 90.0 | 96.03 | 90.8 | 6.6 | 2.6 | ||||||
102.020 | 16-162-12 | 99.0 | 105.04 | 6.3 | 82.9 | 7.2 | 3.5 | |||||
111.770 | 16-162-13 | 108.0 | 115.54 | 92.3 | 5.1 | 2.5 | ||||||
120.770 | 16-162-14 | 117.0 | 124.54 | 47.6 | 52.4 | |||||||
121.205 | 16-162-14 | 117.0 | 125.41 | 3.2 | 91.8 | 3.5 | 1.5 | |||||
128.705 | 16-162-15 | 126.0 | 131.41 | 3.8 | 90.4 | 3.7 | 2.1 | |||||
129.770 | 16-162-15 | 126.0 | 133.54 | 6.7 | 91.2 | 2.1 | ||||||
135.765 | 16-162-16 | 135.0 | 136.53 | 1.4 | 7.0 | 91.6 | ||||||
144.270 | 16-162-17 | 144.0 | 144.54 | 9.0 | 87.9 | 3.1 | ||||||
145.515 | 16-162-17 | 144.0 | 147.03 | 4.0 | 96.0 | |||||||
146.950 | 16-162-17 | 144.0 | 149.90 | 100.0 |