Piskarev, A L; Heunemann, Ch; Makar'ev, A A; Makar'eva, E M; Bachtadse, Valerian; Aleksyutin, M (2009): (Table 3) Magnetic parameters of rocks from the Franz Josef Land archipelago [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.745898, In supplement to: Piskarev, AL et al. (2009): Magnetic parameters and variations in the composition of magmatic rocks from the Franz Josef Land archipelago. Fizika Zemli (Physics of the Earth), No 2, 66-83
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Project(s):
Archive of Ocean Data (ARCOD)
Coverage:
Median Latitude: 80.799861 * Median Longitude: 55.019048 * South-bound Latitude: 79.918900 * West-bound Longitude: 45.081600 * North-bound Latitude: 81.847400 * East-bound Longitude: 63.068100
Event(s):
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 | Sample code/label | Sample label | Piskarev, A L | |||
| 5 | Rock type | Rock | Piskarev, A L | |||
| 6 | Coercivity | Hc | kA/m | Piskarev, A L | ||
| 7 | Coercivity of remanence | Hcr | kA/m | Piskarev, A L | ||
| 8 | Hysteresis, saturation remanence, per unit volume | Msr | mA/m | Piskarev, A L | ||
| 9 | Hysteresis, saturation magnetization, per unit volume | Ms | mA/m | Piskarev, A L | ||
| 10 | Curie temperature | Curie temp | °C | Piskarev, A L | 1 | |
| 11 | Curie temperature | Curie temp | °C | Piskarev, A L | 2 | |
| 12 | NRM, Intensity | Inten (NRM) | mA/m | Piskarev, A L | ||
| 13 | Magnetic susceptibility, volume | kappa | 10-6 SI | Piskarev, A L | ||
| 14 | Factor | Factor | Piskarev, A L | Quality factor | ||
| 15 | Comment | Comment | Piskarev, A L | demagnetization curve type |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
598 data points
Data
| 1 Event | 2 Latitude | 3 Longitude | 4 Sample label | 5 Rock | 6 Hc [kA/m] | 7 Hcr [kA/m] | 8 Msr [mA/m] | 9 Ms [mA/m] | 10 Curie temp [°C] (1) | 11 Curie temp [°C] (2) | 12 Inten (NRM) [mA/m] | 13 kappa [10-6 SI] | 14 Factor (Quality factor) | 15 Comment (demagnetization curve type) |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| FJL-2027-2 | 80.6344 | 53.2257 | 2027-2 | tholeiitic basalt of the oceanic type | 5.9 | 10.3 | 0.4500 | 1.2800 | 162 | 2.05 | 5200 | 9.8 | ||
| FJL-2131tba-1 | 80.1462 | 48.8516 | 2131-5 | tholeiitic basalt of the oceanic type | 17.4 | 6.0 | 0.5300 | 4.4000 | 235 | 560 | 1.38 | 6800 | 5.0 | self-reversal, only one Tc value during cooling |
| FJL-2134-3 | 80.0764 | 50.2560 | 2134-3 | tholeiitic basalt of the oceanic type | 9.1 | 24.8 | 0.7100 | 2.7000 | 237 | 575 | 1.11 | 8000 | 3.4 | 3. |
| FJL-2147 | 79.9189 | 51.0026 | 2147 | tholeiitic basalt of the oceanic type | 1.6 | 5.0 | 0.1000 | 1.5900 | 240 | 0.93 | 10900 | 2.1 | 2. self-reversal | |
| FJL-2147 | 79.9189 | 51.0026 | 2147-2 | tholeiitic basalt of the oceanic type | 11.2 | 20.0 | 1.2000 | 5.7500 | 350 | 500 | 4.20 | 9700 | 10.8 | 4. low Tc, unrecognizable during cooling |
| FJL-2147 | 79.9189 | 51.0026 | 2147-2a | tholeiitic basalt of the oceanic type | 10.6 | 19.7 | 0.6000 | 3.0400 | 340 | 510 | low Tc, unrecognizable during cooling | |||
| FJL-2372 | 80.4509 | 47.4515 | 2372-3 | tholeiitic basalt of the oceanic type | 2.7 | 7.0 | 0.1600 | 0.9200 | 126 | 2.02 | 8900 | 5.7 | ||
| FJL-2372 | 80.4509 | 47.4515 | 2372-5 | tholeiitic basalt of the oceanic type | 5.0 | 15.0 | 0.3300 | 1.9500 | 256 | 465 | 1.56 | 9250 | 4.2 | |
| FJL-3033 | 81.8474 | 59.1553 | 3033 | tholeiitic basalt of the oceanic type | 2.7 | 14.6 | 0.2200 | 1.8700 | 208 | 315 | 1.84 | 14200 | 3.2 | |
| FJL-3069 | 80.3772 | 55.1965 | 3069 | tholeiitic basalt of the oceanic type | 5.2 | 11.8 | 0.3700 | 2.0900 | 262 | 512 | 7.18 | 6400 | 28.0 | 1. |
| FJL-3069 | 80.3772 | 55.1965 | 3069b+ | tholeiitic basalt of the oceanic type | 5.0 | 11.4 | 0.3300 | 1.9000 | 245 | 500 | ||||
| FJL-5017 | 80.7212 | 47.9330 | 5017-6 | tholeiitic basalt of the oceanic type | 10.2 | 30.9 | 0.7200 | 2.2800 | 205 | 513 | 2.61 | 6900 | 9.4 | |
| FJL-5404 | 80.7604 | 49.2286 | 5404-3 | tholeiitic basalt of the oceanic type | 1.9 | 10.1 | 0.5300 | 3.7000 | 170 | 4.80 | 9000 | 13.4 | 1. Tc rise during cooling (>500°C) | |
| FJL-5428 | 80.6905 | 49.6473 | 5428 | tholeiitic basalt of the oceanic type | 7.8 | 13.3 | 1.0400 | 4.4000 | 260 | 500 | 5.22 | 6900 | 18.8 | 1. formation of a new titanomagnetite phase |
| FJL-5428 | 80.6905 | 49.6473 | 5428-3 | tholeiitic basalt of the oceanic type | 6.8 | 13.3 | 1.1000 | 4.4000 | 215 | |||||
| FJL-C-6 | 80.7961 | 47.8961 | C-6 | tholeiitic basalt of the oceanic type | 4.4 | 8.3 | 0.3500 | 2.1000 | 232 | 8.27 | 4600 | 44.0 | 1. | |
| FJL-C-18 | 80.7858 | 47.8603 | C-18 | tholeiitic basalt of the oceanic type | 3.7 | 6.1 | 0.7800 | 5.2000 | 237 | 3.71 | 8800 | 10.6 | 1. formation of a new phase | |
| FJL-C-19 | 80.7858 | 47.8603 | C-19 | tholeiitic basalt of the oceanic type | 2.9 | 7.3 | 0.1900 | 1.0700 | 182 | 3.19 | 11400 | 7.0 | ||
| FJL-46 | 81.0995 | 54.7470 | 46-K | tholeiitic basalt of the transitional type | 4.2 | 18.4 | 0.2400 | 1.9600 | 239 | 612 | 2.40 | 8800 | 6.8 | |
| FJL-2005-1 | 81.2640 | 60.5226 | 2005-1 | tholeiitic basalt of the transitional type | 3.2 | 12.3 | 0.2600 | 3.7000 | 480 | 1.16 | 16300 | 1.8 | 3. self-reversal | |
| FJL-2131tba-2 | 80.1662 | 49.0454 | 2131-3 | tholeiitic basalt of the transitional type | 4.2 | 10.3 | 0.6200 | 3.9000 | 240 | 510 | 1.75 | 14000 | 3.1 | 3. self-reversal, only one Tc value during cooling |
| FJL-2609 | 80.6515 | 63.0681 | 2609-5 | tholeiitic basalt of the transitional type | 3.9 | 16.8 | 0.3200 | 1.7600 | 127 | 1.53 | 19700 | 1.9 | ||
| FJL-2631 | 80.4488 | 46.2080 | 2631-2 | tholeiitic basalt of the transitional type | 10.4 | 14.8 | 0.9700 | 3.0700 | 280 | 500 | 0.87 | 4400 | 4.9 | 1. single Curie point (550°C) during cooling |
| FJL-2711tba-2 | 80.4430 | 60.4319 | 2711-1 | tholeiitic basalt of the transitional type | 4.0 | 10.4 | 0.2500 | 3.8000 | 360 | 490 | 2.63 | 11500 | 5.7 | 3. slightly altered |
| FJL-2832 | 81.7120 | 58.4077 | 2832-1 | tholeiitic basalt of the transitional type | 1.8 | 6.4 | 0.2700 | 4.9000 | 375 | 500 | 0.40 | 8550 | 1.2 | 2. weak second phase |
| FJL-3035 | 81.2928 | 55.5794 | 3035 | tholeiitic basalt of the transitional type | 16.4 | 30.5 | 3.4000 | 14.7000 | 530 | 1.60 | 5150 | 7.8 | 4. | |
| FJL-3674 | 80.8684 | 58.7619 | 3674 | tholeiitic basalt of the transitional type | 3.2 | 10.5 | 0.2800 | 3.1000 | 156 | 443 | 1.72 | 21200 | 2.0 | |
| FJL-5010 | 80.7504 | 48.5803 | 5010-3 | tholeiitic basalt of the transitional type | 15.9 | 27.6 | 1.1000 | 5.2700 | 320 | 580 | 3.22 | 8000 | 10.0 | 3. self-reversal, three phases |
| FJL-D-182 | 80.6121 | 45.0816 | D-182-K | tholeiitic basalt of the transitional type | 21.6 | 41.0 | 1.5500 | 6.9000 | 580 | 3.30 | 9200 | 8.9 | 4. | |
| FJL-2016-3 | 81.0090 | 56.1586 | 2016-3 | tholeiitic basalt of the continental trap type | 13.3 | 21.0 | 0.0980 | 0.3400 | 390 | 570 | 0.19 | 1650 | 2.8 | 2. |
| FJL-2334 | 81.3318 | 54.3098 | 2334-1 | tholeiitic basalt of the continental trap type | 14.7 | 33.4 | 0.4200 | 1.5600 | 532 | 1.50 | 5400 | 7.0 | ||
| FJL-2708 | 80.7845 | 60.6636 | 2708-1 | tholeiitic basalt of the continental trap type | 11.1 | 25.3 | 2.4000 | 15.9000 | 580 | 1.53 | 20500 | 1.8 | 2. | |
| FJL-2711trp | 80.4502 | 60.3246 | 2711-8 | tholeiitic basalt of the continental trap type | 10.4 | 17.3 | 0.2500 | 0.7400 | 345 | 1.38 | 2460 | 14.0 | ||
| FJL-2818trp | 80.1666 | 57.3614 | 2818-1 | tholeiitic basalt of the continental trap type | 10.4 | 17.2 | 0.8600 | 3.0000 | 315 | 575 | 5.37 | 10800 | 12.4 | 2. formation of magnetite during heating |
| FJL-2818trp | 80.1666 | 57.3614 | 2818-5 | tholeiitic basalt of the continental trap type | 6.5 | 21.6 | 0.1060 | 0.5000 | 230 | 0.60 | 2130 | 7.0 | 1. Tc rise during cooling (>500°C) | |
| FJL-2910 | 81.6515 | 62.4362 | 2910-1 | tholeiitic basalt of the continental trap type | 15.8 | 33.0 | 0.9600 | 3.3000 | 566 | 1.92 | 10500 | 4.5 | ||
| FJL-2124 | 81.6879 | 58.1879 | 2124-1 | andesitic basalt | 4.0 | 12.1 | 0.4100 | 3.8000 | 365 | 565 | 1.98 | 17300 | 2.8 | 2. self-reversal |
| FJL-2621 | 81.3988 | 58.4277 | 2621-2 | andesitic basalt | 12.9 | 38.0 | 0.4400 | 2.0200 | 540 | 1.00 | 7050 | 3.5 | ||
| FJL-2818ban | 80.1862 | 57.3591 | 2818-15 | andesitic basalt | 3.8 | 16.7 | 0.1700 | 1.7200 | 323 | 0.50 | 12400 | 1.0 | ||
| FJL-2819ban | 80.1702 | 57.4372 | 2819-3 | andesitic basalt | 2.3 | 10.5 | 0.0500 | 0.8600 | 360 | 450 | 0.41 | 3500 | 2.9 | 1. very weak second phase |
| FJL-3045 | 80.7600 | 57.9513 | 3045II | andesitic basalt | 23.6 | 43.7 | 0.5500 | 1.0100 | 200 | 561 | 9.21 | 2070 | 111.0 | formation of magnetite (Tc, 2) during heating |
| FJL-3045 | 80.7600 | 57.9513 | 3045IIa | andesitic basalt | 10.3 | 5.2300 | 400 | 505 | untypical heating curve | |||||
| FJL-4199 | 80.5383 | 60.3409 | 4199 | andesitic basalt | 8.8 | 18.8 | 1.0500 | 5.1400 | 210 | 500 | 4.06 | 23500 | 4.3 | 2. formation of a new phase |
| FJL-2007 | 81.1417 | 57.0038 | 2007 | andesite | 7.8 | 22.7 | 1.0200 | 10.6000 | 545 | 1.11 | 27800 | 1.0 | 4. | |
| FJL-2320 | 81.1036 | 57.4892 | 2320-3 | andesite | 18.3 | 41.9 | 0.3300 | 0.6500 | 566 | 1.25 | 21000 | 1.4 | 4. self-reversal | |
| FJL-2336 | 81.1959 | 55.7216 | 2336-1 | andesite | 9.0 | 24.5 | 0.7800 | 7.5000 | 570 | 1.74 | 14900 | 2.9 | 4. | |
| FJL-2723 | 81.0701 | 56.2755 | 2723-7 | andesite | 1.6 | 14.2 | 1.1300 | 11.8000 | 370 | 510 | 1.12 | 19600 | 1.4 | |
| FJL-2723 | 81.0701 | 56.2755 | 2723-15 | andesite | 8.7 | 26.7 | 0.5600 | 3.3000 | 180 | 525 | 1.18 | 20800 | 1.4 | |
| FJL-2823 | 80.4392 | 54.1406 | 2823-2 | andesite | 4.9 | 15.5 | 0.2900 | 2.5800 | 275 | 470 | 1.83 | 8500 | 5.4 | 3. very weak second phase |
| FJL-2917 | 81.0768 | 54.3055 | 2917-1 | andesite | 2.0 | 8.5 | 0.2800 | 6.5300 | 350 | 1.69 | 20400 | 2.0 | 3. minor alterations during heating | |
| FJL-2611 | 80.3890 | 60.7057 | 2611-3a | dacite | 251.0 | 200 | 610 | 2.55 | 970 | 66.0 | saturation is not reached | |||
| FJL-2611 | 80.3890 | 60.7057 | 2611-3b | dacite | 200 | 610 | fully reversible thermomagnetic curve | |||||||
| FJL-2319 | 81.2102 | 57.8058 | 2319-2 | dacite | 4.0 | 14.9 | 0.1000 | 1.1956 | 485 | 1.26 | 5930 | 5.3 | 2. hot contact | |
| FJL-2808 | 80.7680 | 60.4157 | 2808-22 | trachybasalt | 3.3 | 20.2 | 0.0084 | 0.0896 | 583 | 0.05 | 1140 | 1.1 | ||
| FJL-2808 | 80.7680 | 60.4157 | 2808-22a | trachybasalt | 4.0 | 14.9 | 0.0390 | 0.2856 | 600 | |||||
| FJL-2811 | 80.9642 | 60.0558 | 2811-1 | trachybasalt | 8.2 | 19.6 | 0.4200 | 2.4528 | 574 | 0.57 | 14200 | 1.0 | 2. |