Shreider, Anatoly A; Trukhin, V I; Sychev, V A; Rimsky-Korsakov, Nikolay A (1982): (Table 1) Magnetic characteristics of samples from the Red Sea rift zone [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.763236, In supplement to: Shreider, AA et al. (1982): Detailed geomagnetic studies of the rift zone in the south of the Red Sea. Translated from Okeanologiya, 1982, 22(3), 325-331, Oceanology, 22(3), 439-445
Always quote citation above when using data! You can download the citation in several formats below.
Project(s):
Archive of Ocean Data (ARCOD)
Coverage:
Median Latitude: 17.964104 * Median Longitude: 40.073812 * South-bound Latitude: 17.931833 * West-bound Longitude: 40.055000 * North-bound Latitude: 17.992167 * East-bound Longitude: 40.094167
Minimum Elevation: -1550.0 m * Maximum Elevation: -1310.0 m
Event(s):
Akvan79/80-53 * Latitude: 17.941833 * Longitude: 40.084000 * Elevation: -1550.0 m * Location: Red Sea * Campaign: PIKAR * Method/Device: Submersible PISCES (PISCES)
Akvan79/80-57 * Latitude: 17.968333 * Longitude: 40.067500 * Elevation: -1310.0 m * Location: Red Sea * Campaign: PIKAR * Method/Device: Submersible PISCES (PISCES)
Akvan79/80-59 * Latitude: 17.971500 * Longitude: 40.064167 * Elevation: -1430.0 m * Location: Red Sea * Campaign: PIKAR * Method/Device: Submersible PISCES (PISCES)
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 | Shreider, Anatoly A | |||
6 | Natural remanent magnetization | NRM | mA/m | Shreider, Anatoly A | ||
7 | Magnetic susceptibility | MAGS | 10-6 SI | Shreider, Anatoly A | ||
8 | Koenigsberger ratio | Q-ratio | A/m | Shreider, Anatoly A |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
108 data points
Data
1 Event | 2 Latitude | 3 Longitude | 4 Elevation [m] | 5 Sample label | 6 NRM [mA/m] | 7 MAGS [10-6 SI] | 8 Q-ratio [A/m] |
---|---|---|---|---|---|---|---|
Akvan79/80-53 | 17.9418 | 40.0840 | -1550 | 53-1a | 4000 | 1.03 | 770 |
Akvan79/80-53 | 17.9418 | 40.0840 | -1550 | 53-1b | 500 | 0.56 | 220 |
Akvan79/80-53 | 17.9418 | 40.0840 | -1550 | 53-1c | 3500 | 1.03 | 655 |
Akvan79/80-53 | 17.9418 | 40.0840 | -1550 | 53-1d | 8500 | 2.79 | 660 |
Akvan79/80-53 | 17.9418 | 40.0840 | -1550 | 53-1e | 700 | 0.72 | 200 |
Akvan79/80-53 | 17.9418 | 40.0840 | -1550 | 53-1f | 200 | 0.40 | 12 |
Akvan79/80-53 | 17.9418 | 40.0840 | -1550 | 53-1g | 21000 | 1.91 | 330 |
Akvan79/80-53 | 17.9418 | 40.0840 | -1550 | 53-1h | 4100 | 15.12 | 375 |
Akvan79/80-53 | 17.9418 | 40.0840 | -1550 | 53-1i | 55000 | 7.96 | 480 |
Akvan79/80-53 | 17.9418 | 40.0840 | -1550 | 53-1j | 70500 | 6.37 | 915 |
Akvan79/80-53 | 17.9418 | 40.0840 | -1550 | 53-1k | 52250 | 5.57 | 670 |
Akvan79/80-57 | 17.9683 | 40.0675 | -1310 | 57a | 46500 | 7.44 | 1280 |
Akvan79/80-59 | 17.9715 | 40.0642 | -1430 | 59-2a | 35000 | 17.59 | 410 |
Akvan79/80-59 | 17.9715 | 40.0642 | -1430 | 59-2b | 19000 | 3.78 | 1035 |
Akvan79/80-59 | 17.9715 | 40.0642 | -1430 | 59-2c | 43000 | 7.24 | 1225 |
Akvan79/80-61 | 17.9463 | 40.0918 | -1510 | 61-1a | 36000 | 6.53 | 1155 |
Akvan79/80-62 | 17.9318 | 40.0942 | -1550 | 62-2a | 69000 | 26.50 | 540 |
Akvan79/80-62 | 17.9318 | 40.0942 | -1550 | 62-2b | 19000 | 3.70 | 1040 |
Akvan79/80-62 | 17.9318 | 40.0942 | -1550 | 62-2c | 73000 | 25.78 | 590 |
Akvan79/80-62 | 17.9318 | 40.0942 | -1550 | 62-2d | 82000 | 32.67 | 520 |
Akvan79/80-62 | 17.9318 | 40.0942 | -1550 | 62-2e | 101000 | 38.16 | 550 |
Akvan79/80-65 | 17.9922 | 40.0738 | -1500 | 65-1a | 63500 | 4.81 | 2730 |
Akvan79/80-65 | 17.9922 | 40.0738 | -1500 | 65-1b | 36000 | 3.98 | 1880 |
Akvan79/80-66 | 17.9817 | 40.0600 | -1410 | 66-4a | 56500 | 13.53 | 860 |
Akvan79/80-66 | 17.9817 | 40.0600 | -1410 | 66-4b | 47500 | 28.25 | 350 |
Akvan79/80-66 | 17.9817 | 40.0600 | -1410 | 66-4c | 36000 | 19.50 | 385 |
Akvan79/80-67 | 17.9792 | 40.0550 | -1540 | 67 | 37000 | 10.35 | 370 |