Sato, Hiroaki (1989): (Table 2) Mineral composition of experiments on basalt samples of ODP Hole 111-504B [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.749718, In supplement to: Sato, H (1989): Mg-Fe partitioning between plagioclase and liquid in basalts of Hole 504B, ODP Leg 111: a study of melting at 1 ATM. In: Becker, K; Sakai, H; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 111, 17-26, https://doi.org/10.2973/odp.proc.sr.111.113.1989
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Project(s):
Ocean Drilling Program (ODP)
Coverage:
Latitude: 1.226900 * Longitude: -83.730300
Date/Time Start: 1986-10-05T11:45:00 * Date/Time End: 1986-10-16T18:15:00
Minimum Elevation: -3474.0 m * Maximum Elevation: -3474.0 m
Event(s):
111-504B * Latitude: 1.226900 * Longitude: -83.730300 * Date/Time Start: 1986-10-05T11:45:00 * Date/Time End: 1986-10-16T18:15:00 * Elevation: -3474.0 m * Penetration: 1562.1 m * Recovery: 27.36 m * Location: North Pacific Ocean * Campaign: Leg111 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 29 cores; 209 m cored; 0 m drilled; 13.1 % recovery
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Sample code/label | Sample label | Sato, Hiroaki | DSDP/ODP/IODP sample designation | ||
| 2 | Number | No | Sato, Hiroaki | piece | ||
| 3 | Sample comment | Sample comment | Sato, Hiroaki | |||
| 4 | Temperature, technical | T tech | °C | Sato, Hiroaki | ||
| 5 | - | - | Sato, Hiroaki | Log f(O2) | ||
| 6 | Duration | Duration | h | Sato, Hiroaki | ||
| 7 | Volcanic glass | Volc glass | % | Sato, Hiroaki | ||
| 8 | Plagioclase | Pl | % | Sato, Hiroaki | calcium-rich | |
| 9 | Olivine | Ol | % | Sato, Hiroaki | ||
| 10 | Clinopyroxene | Cpx | % | Sato, Hiroaki | ||
| 11 | Magnetite | Fe3O4 | % | Sato, Hiroaki |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
638 data points
Data
| 1 Sample label | 2 No | 3 Sample comment | 4 T tech [°C] | 5 - | 6 Duration [h] | 7 Volc glass [%] | 8 Pl [%] | 9 Ol [%] | 10 Cpx [%] | 11 Fe3O4 [%] |
|---|---|---|---|---|---|---|---|---|---|---|
| 111-504B-143R-2 | 8 | 4A | 1200 | -8.0 | 9.0 | 60 | 20 | 0 | 20 | 0 |
| 111-504B-143R-2 | 8 | 5A | 1250 | -8.0 | 1.0 | >99 | <1 | 0 | 0 | 0 |
| 111-504B-143R-2 | 8 | 6A | 1240 | -8.0 | 2.1 | 99 | 1 | 0 | 0 | 0 |
| 111-504B-143R-2 | 8 | 8A | 1180 | -8.0 | 13.0 | 30 | 40 | 0 | 30 | 0 |
| 111-504B-143R-2 | 8 | 9A | 1230 | -8.0 | 1.4 | 90 | 10 | 0 | <1 | 0 |
| 111-504B-143R-2 | 8 | 10A | 1220 | -8.0 | 1.0 | 75 | 20 | 0 | 5 | 0 |
| 111-504B-143R-2 | 8 | 12A | 1150 | -8.0 | 9.2 | 10 | 50 | 0 | 40 | 0 |
| 111-504B-143R-2 | 8 | 13A | 1210 | -8.0 | 12.3 | 60 | 30 | ?0 | 10 | 0 |
| 111-504B-143R-2 | 8 | 14A | 1190 | -8.0 | 10.6 | 40 | 40 | 0 | 20 | 0 |
| 111-504B-143R-2 | 8 | 22A | 1255 | -8.0 | 3.5 | 100 | 0 | 0 | 0 | 0 |
| 111-504B-143R-2 | 8 | 43A | 1300 | -0.7 | 0.6 | 100 | 0 | 0 | 0 | 0 |
| 111-504B-143R-2 | 8 | 15A | 1220 | -8.0 | 47.4 | 98 | 2 | 0 | 0 | 0 |
| 111-504B-143R-2 | 8 | 16A | 1200 | -8.0 | 73.0 | 77 | 20 | 3 | 0 | 0 |
| 111-504B-143R-2 | 8 | 17A | 1240 | -8.0 | 35.1 | 100 | 0 | 0 | 0 | 0 |
| 111-504B-143R-2 | 8 | 19A | 1230 | -8.0 | 23.6 | 100 | 0 | 0 | 0 | 0 |
| 111-504B-143R-2 | 8 | 24A | 1210 | -8.0 | 25.0 | 99 | 1 | 0 | 0 | 0 |
| 111-504B-143R-2 | 8 | 25A | 1240 | -6.0 | 13.0 | 100 | 0 | 0 | 0 | 0 |
| 111-504B-143R-2 | 8 | 26A | 1220 | -6.0 | 19.5 | 95 | 5 | 0 | 0 | 0 |
| 111-504B-143R-2 | 8 | 34A | 1180 | -8.8 | 24.7 | 73 | 20 | 5 | 2 | 0 |
| 111-504B-143R-2 | 8 | 35A | 1200 | -10.0 | 32.1 | 88 | 10 | 2 | 0 | 0 |
| 111-504B-143R-2 | 8 | 41A | 1220 | -9.7 | 26.4 | 99 | 1 | 0 | 0 | 0 |
| 111-504B-143R-2 | 8 | 42A | 1220 | -7.0 | 34.5 | 100 | 0 | 0 | 0 | 0 |
| 111-504B-143R-2 | 8 | 45A | 1220 | -9.0 | 39.5 | >99 | <1 | 0 | 0 | 0 |
| 111-504B-143R-2 | 8 | 46A | 1220 | -8.0 | 39.5 | >99 | <1 | 0 | 0 | 0 |
| 111-504B-143R-2 | 8 | 48A | 1230 | -8.0 | 24.4 | 100 | 0 | 0 | 0 | 0 |
| 111-504B-143R-2 | 8 | 50A | 1200 | -0.7 | 42.9 | 83 | 15 | 0 | 0 | 2 |
| 111-504B-143R-2 | 8 | 51A | 1200 | -3.9 | 42.1 | 84 | 15 | 0 | 0 | 1 |
| 111-504B-143R-2 | 8 | 52A | 1200 | -7.0 | 42.9 | 85 | 15 | 0 | 0 | <1 |
| 111-504B-143R-2 | 8 | 79A | 1200 | -11.5 | 97.5 | 78 | 20 | 2 | 0 | 0 |
| 111-504B-169R-1 | 1 | 3B | 1240 | -7.5 | 3.4 | 100 | 0 | 0 | 0 | 0 |
| 111-504B-169R-1 | 1 | 4B | 1200 | -8.0 | 9.0 | 82 | 15 | 0 | 3 | 0 |
| 111-504B-169R-1 | 1 | 8B | 1180 | -8.0 | 13.0 | 60 | 30 | 0 | 10 | 0 |
| 111-504B-169R-1 | 1 | 09B | 1230 | -8.0 | 1.4 | 99 | 1 | 0 | 0 | 0 |
| 111-504B-169R-1 | 1 | 10B | 1220 | -8.0 | 1.0 | 95 | 5 | 0 | 0 | 0 |
| 111-504B-169R-1 | 1 | 11B | 1210 | -8.0 | 2.8 | 93 | 7 | 0 | 0 | 0 |
| 111-504B-169R-1 | 1 | 12B | 1150 | -8.0 | 9.2 | 10 | 50 | 0 | 40 | 0 |
| 111-504B-169R-1 | 1 | 13B | 1210 | -8.0 | 12.3 | 95 | 5 | ?0 | 0 | 0 |
| 111-504B-169R-1 | 1 | 14B | 1190 | -8.0 | 10.6 | 60 | 30 | 0 | 10 | 0 |
| 111-504B-169R-1 | 1 | 44B | 1300 | -0.7 | 0.4 | 100 | 0 | 0 | 0 | 0 |
| 111-504B-169R-1 | 1 | 5B | 1220 | -8.0 | 47.4 | 100 | 0 | 0 | 0 | 0 |
| 111-504B-169R-1 | 1 | 16B | 1200 | -8.0 | 73.0 | 95 | 5 | 0 | 0 | 0 |
| 111-504B-169R-1 | 1 | 18B | 1240 | -8.0 | 31.5 | 100 | 0 | 0 | 0 | 0 |
| 111-504B-169R-1 | 1 | 19B | 1230 | -8.0 | 23.6 | 100 | 0 | 0 | 0 | 0 |
| 111-504B-169R-1 | 1 | 24B | 1210 | -8.0 | 25.0 | 100 | 0 | 0 | 0 | 0 |
| 111-504B-169R-1 | 1 | 26B | 1220 | -6.0 | 19.5 | 100 | 0 | 0 | 0 | 0 |
| 111-504B-169R-1 | 1 | 34B | 1180 | -8.8 | 24.7 | 95 | 5 | 0 | 0 | 0 |
| 111-504B-169R-1 | 1 | 35B | 1200 | -10.0 | 32.1 | 99 | 1 | 0 | 0 | 0 |
| 111-504B-169R-1 | 1 | 39B | 1250 | -8.0 | 25.1 | 100 | 0 | 0 | 0 | 0 |
| 111-504B-169R-1 | 1 | 41B | 1220 | -9.7 | 26.4 | 100 | 0 | 0 | 0 | 0 |
| 111-504B-169R-1 | 1 | 42B | 1220 | -7.0 | 34.5 | 100 | 0 | 0 | 0 | 0 |
| 111-504B-169R-1 | 1 | 45B | 1220 | -9.0 | 39.5 | 100 | 0 | 0 | 0 | 0 |
| 111-504B-169R-1 | 1 | 46B | 1220 | -8.0 | 39.5 | 100 | 0 | 0 | 0 | 0 |
| 111-504B-169R-1 | 1 | 47B | 1200 | -8.0 | 23.0 | >99 | <1 | 0 | 0 | 0 |
| 111-504B-169R-1 | 1 | 48B | 1230 | -8.0 | 24.4 | 100 | 0 | 0 | 0 | 0 |
| 111-504B-169R-1 | 1 | 50B | 1200 | -0.7 | 42.9 | 93 | 5 | 0 | 0 | 2 |
| 111-504B-169R-1 | 1 | 51B | 1200 | -3.9 | 42.1 | 97 | 3 | 0 | 0 | <1 |
| 111-504B-169R-1 | 1 | 52B | 1200 | -7.0 | 42.9 | 98 | 2 | 0 | 0 | <1 |
| 111-504B-169R-1 | 1 | 79B | 1200 | -11.5 | 97.5 | 98 | 2 | 0 | 0 | 0 |