Joseph, Leah H; Rea, David K; van der Pluijm, Ben A (1998): (Table B) Results of analysis of Bermuda Rise sediment core CH89-9P [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.857862, In supplement to: Joseph, LH et al. (1998): Use of grain size and magnetic fabric analyses to distinguish among depositional environments. Paleoceanography, 13(5), 491-501, https://doi.org/10.1029/98PA01939
Always quote citation above when using data! You can download the citation in several formats below.
Other version:
Joseph, Leah H; Rea, David K; van der Pluijm, Ben A (2003): NOAA/WDS Paleoclimatology - Grain Size and Magnetic Fabric Data. NOAA National Centers for Environmental Information, https://doi.org/10.25921/C02Y-TF55
Coverage:
Latitude: 33.690000 * Longitude: -57.620000
Minimum DEPTH, sediment/rock: 0.490 m * Maximum DEPTH, sediment/rock: 18.915 m
Event(s):
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Joseph, Leah H | Geocode | |
| 2 | Size | Size | µm | Joseph, Leah H | ||
| 3 | Size | Size | µm | Joseph, Leah H | #2 | |
| 4 | Standard deviation | Std dev | ± | Joseph, Leah H | IGSD = inclusive graphic standard deviation | |
| 5 | Standard deviation | Std dev | ± | Joseph, Leah H | IGSD = inclusive graphic standard deviation, #2 | |
| 6 | Magnitude of anisotropy | P` | Joseph, Leah H | strength of anisotropy | ||
| 7 | Shape of susceptibility | T | Joseph, Leah H | shape of anisotropy | ||
| 8 | Magnetic susceptibility | MAGS | 10-6 SI | Joseph, Leah H | ||
| 9 | Magnetic susceptibility | MAGS | 10-6 SI | Joseph, Leah H | susceptibilities of a halved cube at 298 | |
| 10 | Magnetic susceptibility | MAGS | 10-6 SI | Joseph, Leah H | susceptibilities of a halved cube at 77 |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
432 data points