Smirnov, Alexei; Tarduno, John A (2003): (Table 1) Magnetic hysteresis parameters for samples from ODP Hole 197-1203A [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.721004, In supplement to: Smirnov, A; Tarduno, JA (2003): Magnetic hysteresis monitoring of Cretaceous submarine basaltic glass during Thellier paleointensity experiments: evidence for alteration and attendant low field bias. Earth and Planetary Science Letters, 206(3-4), 571-585, https://doi.org/10.1016/S0012-821X(02)01123-8
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Project(s):
Ocean Drilling Program (ODP)
Coverage:
Latitude: 50.949960 * Longitude: 167.739950
Date/Time Start: 2001-07-11T00:00:00 * Date/Time End: 2001-07-11T00:00:00
Minimum DEPTH, sediment/rock: 458.45 m * Maximum DEPTH, sediment/rock: 621.46 m
Event(s):
197-1203A * Latitude: 50.949960 * Longitude: 167.739950 * Date/Time: 2001-07-11T00:00:00 * Elevation: -2593.5 m * Penetration: 914.6 m * Recovery: 333.91 m * Location: North Pacific Ocean * Campaign: Leg197 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 68 cores; 614.6 m cored; 300 m drilled; 54.3 % recovery
Comment:
The signal/noise ratio (defined as the ratio of the total Ms to the Ms of the AGFM P1-type probe) is larger than five for all data points
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
2 | Coercivity | Hc | mT | Smirnov, Alexei | Alternating Gradient Force Magnetometer (AGFM) | |
3 | Coercivity of remanence | Bcr | mT | Smirnov, Alexei | Alternating Gradient Force Magnetometer (AGFM) | |
4 | Hysteresis, saturation magnetization/ saturation remanence | Mrs/Ms | Smirnov, Alexei | Alternating Gradient Force Magnetometer (AGFM) |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
48 data points
Data
1 Depth sed [m] | 2 Hc [mT] | 3 Bcr [mT] | 4 Mrs/Ms |
---|---|---|---|
458.45 | 33.6 | 94.3 | 0.334 |
464.41 | 34.0 | 94.0 | 0.334 |
465.00 | 28.6 | 103.0 | 0.301 |
465.07 | 29.8 | 99.9 | 0.313 |
465.32 | 27.5 | 82.8 | 0.273 |
465.40 | 22.9 | 75.4 | 0.308 |
466.70 | 29.5 | 91.8 | 0.295 |
466.75 | 27.7 | 109.0 | 0.239 |
475.68 | 15.3 | 54.0 | 0.180 |
479.19 | 24.6 | 73.1 | 0.279 |
579.61 | 35.0 | 81.7 | 0.289 |
580.17 | 31.4 | 75.7 | 0.337 |
580.52 | 17.4 | 80.9 | 0.159 |
621.06 | 47.0 | 106.0 | 0.362 |
621.06 | 59.6 | 109.0 | 0.442 |
621.46 | 26.7 | 89.7 | 0.270 |