Dmitriev, Yuri I (1982): (Table 7) Chemical composition of olivine-plagioclase phyric and plagioclase phyric basalts at DSDP Sites 67-495 and 67-500 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.817490, In supplement to: Dmitriev, YI (1982): Basalts of the Middle America Trench (Guatemala Transect) and their correlation with oceanic and island-arc tholeiites. In: Abouin, J; von Huene, R; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 67, 577-584, https://doi.org/10.2973/dsdp.proc.67.124.1982
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Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Median Latitude: 12.623233 * Median Longitude: -90.974067 * South-bound Latitude: 12.496300 * West-bound Longitude: -91.037700 * North-bound Latitude: 12.689200 * East-bound Longitude: -90.941500
Date/Time Start: 1979-05-26T00:00:00 * Date/Time End: 1979-06-18T00:00:00
Minimum Elevation: -6094.0 m * Maximum Elevation: -4140.0 m
Event(s):
67-495 * Latitude: 12.496300 * Longitude: -91.037700 * Date/Time: 1979-05-26T00:00:00 * Elevation: -4140.0 m * Penetration: 455.5 m * Recovery: 333.7 m * Location: North Pacific/TRENCH * Campaign: Leg67 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 48 cores; 446 m cored; 9.5 m drilled; 74.8 % recovery
67-500 * Latitude: 12.689200 * Longitude: -90.941500 * Date/Time: 1979-06-18T00:00:00 * Elevation: -6094.0 m * Penetration: 165.5 m * Recovery: 73.3 m * Location: North Pacific/TRENCH * Campaign: Leg67 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 18 cores; 156 m cored; 9.5 m drilled; 47 % recovery
67-500B * Latitude: 12.684200 * Longitude: -90.943000 * Date/Time: 1979-06-18T00:00:00 * Elevation: -6090.0 m * Penetration: 133.5 m * Recovery: 16.8 m * Location: North Pacific/TRENCH * Campaign: Leg67 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 3 cores; 28.5 m cored; 0 m drilled; 58.8 % recovery
Comment:
Empty cells indicates that analysis for this component was not carried out.
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | Event label | Event | ||||
2 | Latitude of event | Latitude | ||||
3 | Longitude of event | Longitude | ||||
4 | Elevation of event | Elevation | m | |||
5 | Sample code/label | Sample label | Dmitriev, Yuri I | DSDP/ODP/IODP sample designation | ||
6 | Comment | Comment | Dmitriev, Yuri I | |||
7 | Description | Description | Dmitriev, Yuri I | |||
8 | Identification | ID | Dmitriev, Yuri I | |||
9 | Silicon dioxide | SiO2 | % | Dmitriev, Yuri I | ||
10 | Titanium dioxide | TiO2 | % | Dmitriev, Yuri I | ||
11 | Aluminium oxide | Al2O3 | % | Dmitriev, Yuri I | ||
12 | Iron oxide, Fe2O3 | Fe2O3 | % | Dmitriev, Yuri I | ||
13 | Iron oxide, FeO | FeO | % | Dmitriev, Yuri I | ||
14 | Manganese oxide | MnO | % | Dmitriev, Yuri I | ||
15 | Magnesium oxide | MgO | % | Dmitriev, Yuri I | ||
16 | Calcium oxide | CaO | % | Dmitriev, Yuri I | ||
17 | Sodium oxide | Na2O | % | Dmitriev, Yuri I | ||
18 | Potassium oxide | K2O | % | Dmitriev, Yuri I | ||
19 | Water in rock | H2O | % | Dmitriev, Yuri I | H2O-, hydration part | |
20 | Water in rock | H2O | % | Dmitriev, Yuri I | H2O+, structural part, similar to LOI | |
21 | Phosphorus pentoxide | P2O5 | % | Dmitriev, Yuri I | ||
22 | Carbon dioxide | CO2 | % | Dmitriev, Yuri I | ||
23 | Sulfur, total | TS | % | Dmitriev, Yuri I | ||
24 | Fluorine | F | % | Dmitriev, Yuri I | ||
25 | Chlorine | Cl | % | Dmitriev, Yuri I | ||
26 | Chromium(III) oxide | Cr2O3 | % | Dmitriev, Yuri I | ||
27 | Vanadium oxide | V2O5 | % | Dmitriev, Yuri I | ||
28 | Lithium oxide | Li2O | % | Dmitriev, Yuri I | ||
29 | Rubidium oxide | Rb2O | % | Dmitriev, Yuri I | ||
30 | Caesium oxide | Cs2O | % | Dmitriev, Yuri I | ||
31 | Total | Total | % | Dmitriev, Yuri I |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
154 data points
Data
1 Event | 2 Latitude | 3 Longitude | 4 Elevation [m] | 5 Sample label | 6 Comment | 7 Description | 8 ID | 9 SiO2 [%] | 10 TiO2 [%] | 11 Al2O3 [%] | 12 Fe2O3 [%] | 13 FeO [%] | 14 MnO [%] | 15 MgO [%] | 16 CaO [%] | 17 Na2O [%] | 18 K2O [%] | 19 H2O [%] (H2O-, hydration part) | 20 H2O [%] (H2O+, structural part, simila...) | 21 P2O5 [%] | 22 CO2 [%] | 23 TS [%] | 24 F [%] | 25 Cl [%] | 26 Cr2O3 [%] | 27 V2O5 [%] | 28 Li2O [%] | 29 Rb2O [%] | 30 Cs2O [%] | 31 Total [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
67-495 | 12.4963 | -91.0377 | -4140 | 67-495-48-1,83 | From beginning of section | Olivine-plagioclase phyric basalts | 1 | 45.8 | 1.47 | 15.15 | 6.03 | 3.80 | 0.21 | 5.05 | 13.94 | 3.02 | 0.320 | 0.32 | 2.08 | 0.18 | 2.11 | 0.04 | 0.07 | 0.05 | 0.05 | 0.0050 | 0.0009 | 0.0021 | 100.20 | |
67-495 | 12.4963 | -91.0377 | -4140 | 67-495-48-4,93 | Olivine-plagioclase phyric basalts | 2 | 49.2 | 1.51 | 15.60 | 2.72 | 7.27 | 0.16 | 7.24 | 11.58 | 2.98 | 0.075 | 0.52 | 1.08 | 0.19 | 0.10 | 0.03 | 0.06 | 0.05 | 0.05 | 0.0016 | 0.0007 | 0.0002 | 100.42 | ||
67-500 | 12.6892 | -90.9415 | -6094 | 67-500-18-1,36 | Olivine-plagioclase phyric basalts | 3 | 48.2 | 1.81 | 16.80 | 3.61 | 6.29 | 0.12 | 5.70 | 11.07 | 3.01 | 0.630 | 0.60 | 1.71 | 0.26 | 0.42 | 0.02 | 0.04 | 0.06 | 0.03 | 0.05 | 0.0017 | 0.0018 | 0.0002 | 100.44 | |
67-500B | 12.6842 | -90.9430 | -6090 | 67-500B-3-1,64 | Olivine-plagioclase phyric basalts | 4 | 50.1 | 1.18 | 15.30 | 2.06 | 6.69 | 0.17 | 8.67 | 11.16 | 2.31 | 0.053 | 0.00 | 1.95 | 0.10 | 0.24 | 0.07 | 0.04 | 0.04 | 0.06 | 0.05 | 0.0033 | 0.0005 | 0.0002 | 100.24 | |
67-500 | 12.6892 | -90.9415 | -6094 | 67-500-19-1,9 | Plagioclase phyric basalts | 6 | 47.5 | 1.27 | 20.55 | 6.47 | 3.08 | 0.07 | 3.42 | 11.17 | 2.90 | 0.720 | 0.72 | 1.68 | 0.25 | 0.18 | 0.06 | 0.04 | 0.15 | 0.09 | 0.05 | 0.0011 | 0.0010 | 0.0028 | 100.37 | |
67-500 | 12.6892 | -90.9415 | -6094 | 67-500-19-1,52 | Plagioclase phyric basalts | 7 | 48.0 | 1.74 | 17.55 | 3.60 | 5.31 | 0.12 | 6.50 | 11.18 | 2.88 | 0.420 | 0.35 | 2.03 | 0.25 | 0.03 | 0.04 | 0.04 | 0.05 | 0.06 | 0.0012 | 0.0010 | 0.0002 | 100.15 |