Ryan, William B F; Hsü, Kenneth J (2004): Mineral composition of silt fraction from Hole 13-132 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.220018
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
Kaneps, Ansis G; Wezel, Forese C; Stradner, Herbert; Pautot, Guy; Nesteroff, Wladimir D; Maync, Wolf; Llort, Jennifer; Dumitrica, Paulian; Cita, Maria Bianca; Ryan, William B F; Hsü, Kenneth J (1973): Initial Reports of the Deep Sea Drilling Project 13. Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, XIII, 514 pp, https://doi.org/10.2973/dsdp.proc.13.1973
Further details:
X-ray mineralogy data base - Background and methods. hdl:10013/epic.32358.d001
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: 40.261700 * Longitude: 11.441200
Date/Time Start: 1970-09-24T00:00:00 * Date/Time End: 1970-09-24T00:00:00
Minimum DEPTH, sediment/rock: 0.075 m * Maximum DEPTH, sediment/rock: 221.285 m
Event(s):
13-132 * Latitude: 40.261700 * Longitude: 11.441200 * Date/Time: 1970-09-24T00:00:00 * Elevation: -2835.0 m * Penetration: 223 m * Recovery: 165.3 m * Location: Mediterranean Sea/CONT RISE * Campaign: Leg13 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 26 cores; 214 m cored; 9 m drilled; 77.2 % 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 | Amphibole | Amp | % | X-ray diffraction, silt fraction | ||
6 | Analcite | Anl | % | X-ray diffraction, silt fraction | ||
7 | Augite | Aug | % | X-ray diffraction, silt fraction | ||
8 | Chlorite | Chl | % | X-ray diffraction, silt fraction | ||
9 | Dolomite | Dol | % | X-ray diffraction, silt fraction | ||
10 | Hematite, Fe2O3 | Hem | % | X-ray diffraction, silt fraction | ||
11 | Kaolinite | Kln | % | X-ray diffraction, silt fraction | ||
12 | Kalifeldspar | Kfs | % | X-ray diffraction, silt fraction | ||
13 | Mica | Mica | % | X-ray diffraction, silt fraction | ||
14 | Palygorskite | Plg | % | X-ray diffraction, silt fraction | ||
15 | Phillipsite | Php | % | X-ray diffraction, silt fraction | ||
16 | Plagioclase | Pl | % | X-ray diffraction, silt fraction | ||
17 | Quartz | Qz | % | X-ray diffraction, silt fraction |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
332 data points
Data
1 Depth sed [m] | 2 Sample label | 3 Depth top [m] | 4 Depth bot [m] | 5 Amp [%] | 6 Anl [%] | 7 Aug [%] | 8 Chl [%] | 9 Dol [%] | 10 Hem [%] | 11 Kln [%] | 12 Kfs [%] | 13 Mica [%] | 14 Plg [%] | 15 Php [%] | 16 Pl [%] | 17 Qz [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
0.075 | 13-132-1 | 0.0 | 0.15 | 4.5 | 7.9 | 45.9 | 16.0 | 1.1 | 24.7 | |||||||
1.025 | 13-132-1 | 0.0 | 2.05 | 3.1 | 3.5 | 3.3 | 3.5 | 36.1 | 6.2 | 9.8 | 34.4 | |||||
1.680 | 13-132-1 | 0.0 | 3.36 | 50.0 | 3.1 | 24.4 | 8.0 | 14.0 | ||||||||
1.950 | 13-132-1 | 0.0 | 3.90 | 4.7 | 4.6 | 37.8 | 13.5 | 39.3 | ||||||||
3.550 | 13-132-1 | 0.0 | 7.10 | 1.1 | 4.3 | 2.8 | 31.7 | 15.9 | 44.3 | |||||||
9.935 | 13-132-2 | 9.0 | 10.87 | 1.2 | 5.2 | 2.8 | 35.6 | 15.0 | 40.2 | |||||||
11.765 | 13-132-2 | 9.0 | 14.53 | 1.8 | 3.7 | 4.3 | 30.8 | 16.1 | 43.3 | |||||||
18.700 | 13-132-3 | 18.0 | 19.40 | 1.8 | 18.4 | 9.7 | 46.6 | 2.6 | 20.9 | |||||||
27.920 | 13-132-4 | 27.0 | 28.84 | 1.4 | 3.8 | 4.2 | 2.7 | 26.4 | 17.5 | 44.1 | ||||||
29.825 | 13-132-4 | 27.0 | 32.65 | 3.6 | 6.7 | 37.2 | 14.1 | 38.3 | ||||||||
31.050 | 13-132-4 | 27.0 | 35.10 | 3.6 | 5.1 | 31.5 | 12.0 | 47.8 | ||||||||
37.290 | 13-132-5 | 36.0 | 38.58 | 3.0 | 2.1 | 8.2 | 31.3 | 19.5 | 35.7 | |||||||
46.980 | 13-132-6 | 45.0 | 48.96 | 1.0 | 3.2 | 5.8 | 3.4 | 29.0 | 10.0 | 12.1 | 35.5 | |||||
47.750 | 13-132-6 | 45.0 | 50.50 | 4.3 | 3.0 | 30.7 | 13.7 | 48.4 | ||||||||
54.245 | 13-132-7 | 54.0 | 54.49 | 3.5 | 4.2 | 5.8 | 29.3 | 14.4 | 42.3 | |||||||
57.450 | 13-132-7 | 54.0 | 60.90 | 4.9 | 5.2 | 33.5 | 12.7 | 43.6 | ||||||||
66.275 | 13-132-8 | 63.0 | 69.55 | 5.2 | 1.4 | 3.8 | 24.1 | 17.2 | 48.3 | |||||||
74.630 | 13-132-9 | 72.0 | 77.26 | 5.1 | 3.1 | 33.9 | 14.7 | 43.1 | ||||||||
82.500 | 13-132-10 | 81.0 | 84.00 | 2.8 | 3.8 | 5.8 | 27.7 | 14.1 | 45.1 | |||||||
93.200 | 13-132-11 | 90.0 | 96.40 | 2.9 | 3.1 | 10.0 | 28.0 | 15.4 | 40.5 | |||||||
101.225 | 13-132-12 | 99.0 | 103.45 | 4.0 | 4.1 | 36.4 | 14.8 | 40.6 | ||||||||
109.000 | 13-132-13 | 108.0 | 110.00 | 4.7 | 5.5 | 4.9 | 35.5 | 11.6 | 37.8 | |||||||
118.265 | 13-132-14 | 117.0 | 119.53 | 4.0 | 7.0 | 36.0 | 10.5 | 42.5 | ||||||||
128.450 | 13-132-15 | 126.0 | 130.90 | 3.3 | 2.6 | 6.5 | 29.8 | 11.2 | 46.7 | |||||||
136.990 | 13-132-16 | 135.0 | 138.98 | 3.9 | 5.6 | 3.6 | 27.3 | 11.5 | 48.2 | |||||||
145.430 | 13-132-17 | 144.0 | 146.86 | 6.0 | 4.6 | 32.3 | 12.1 | 45.0 | ||||||||
155.775 | 13-132-18 | 153.0 | 158.55 | 4.2 | 5.6 | 4.6 | 33.7 | 12.3 | 39.7 | |||||||
163.250 | 13-132-19 | 162.0 | 164.50 | 5.3 | 1.0 | 5.4 | 33.5 | 10.9 | 43.8 | |||||||
164.175 | 13-132-19 | 162.0 | 166.35 | 4.4 | 5.6 | 31.2 | 9.9 | 48.8 | ||||||||
172.475 | 13-132-20 | 171.0 | 173.95 | 3.3 | 6.7 | 4.3 | 30.8 | 8.4 | 46.5 | |||||||
173.330 | 13-132-20 | 171.0 | 175.66 | 5.0 | 1.4 | 4.7 | 33.6 | 8.3 | 47.1 | |||||||
173.500 | 13-132-20 | 171.0 | 176.00 | 5.5 | 3.2 | 43.4 | 10.5 | 37.3 | ||||||||
180.300 | 13-132-21 | 180.0 | 180.60 | 5.0 | 3.1 | 45.9 | 9.5 | 36.5 | ||||||||
180.765 | 13-132-21 | 180.0 | 181.53 | 4.5 | 8.0 | 39.7 | 9.5 | 38.4 | ||||||||
181.400 | 13-132-21 | 180.0 | 182.80 | 4.4 | 4.6 | 3.1 | 42.6 | 9.2 | 36.1 | |||||||
207.325 | 13-132-25 | 207.0 | 207.65 | 5.7 | 5.6 | 4.4 | 36.1 | 10.4 | 37.9 | |||||||
208.200 | 13-132-25 | 207.0 | 209.40 | 9.0 | 3.8 | 33.0 | 10.3 | 43.8 | ||||||||
221.285 | 13-132-27 | 220.0 | 222.57 | 7.2 | 5.9 | 5.4 | 30.5 | 8.2 | 42.8 |