Westerhold, Thomas; Röhl, Ursula; Pälike, Heiko; Wilkens, Roy H; Wilson, Paul A; Acton, Gary D (2013): (Table S17) U-channel paleomagnetic data of IODP Hole 320-U1333A [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.825689, In supplement to: Westerhold, T et al. (2014): Orbitally tuned timescale and astronomical forcing in the middle Eocene to early Oligocene. Climate of the Past, 10, 955-973, https://doi.org/10.5194/cp-10-955-2014
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Project(s):
Coverage:
Latitude: 10.516580 * Longitude: -138.419540
Minimum DEPTH, sediment/rock: 85.54 m * Maximum DEPTH, sediment/rock: 95.00 m
Event(s):
320-U1333A * Latitude: 10.516580 * Longitude: -138.419540 * Elevation: -4853.7 m * Recovery: 176.25 m * Campaign: Exp320 (Pacific Equatorial Age Transect I) * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 22 cores; 184.1 m cored; 95.7 % recovered; 0 m drilled; 184.1 m penetrated
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | Sample code/label | Sample label | Acton, Gary D | |||
2 | Interval Cored | Cored | m | Acton, Gary D | ||
3 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
4 | Depth, composite | Depth comp | mcd | Acton, Gary D | based on Table 8 of Westerhold et al. (2012), CCSF-A | |
5 | Depth, composite revised, adjusted | Depth adj rmcd | armcd | Acton, Gary D | based on Table 10 of Westerhold et al. (2012) | |
6 | AGE | Age | ka BP | Geocode | ||
7 | Half | Half | Acton, Gary D | working or archive half | ||
8 | Filter | Filter | Acton, Gary D | data filter 1, If =0, data are suspect | ||
9 | Filter | Filter | Acton, Gary D | data filter 2, If =0, data are suspect | ||
10 | Natural remanent magnetization | NRM | mT | Acton, Gary D | no demagnetization, (AFD000) | |
11 | NRM, Declination | Decl (NRM) | deg | Acton, Gary D | no demagnetization, (Dec000) | |
12 | NRM, Inclination | Incl (NRM) | deg | Acton, Gary D | no demagnetization, (Inc000) | |
13 | NRM, Intensity | Inten (NRM) | mA/m | Acton, Gary D | NRM magnetization with no demagnetization, (Int000) | |
14 | Natural remanent magnetization | NRM | mT | Acton, Gary D | 20 mT AF demagnetization, (AFD020) | |
15 | NRM, Declination after demagnetization | Decl (AF) | deg | Acton, Gary D | 20 mT AF demagnetization, (Dec020) | |
16 | NRM, Inclination after demagnetization | Incl (AF) | deg | Acton, Gary D | 20 mT AF demagnetization, (Inc020) | |
17 | NRM, Intensity | Inten (NRM) | mA/m | Acton, Gary D | NRM magnetization with 20 mT AF demagnetization (Int020) | |
18 | Natural remanent magnetization | NRM | mT | Acton, Gary D | 25 mT AF demagnetization, (AFD025) | |
19 | NRM, Declination after demagnetization | Decl (AF) | deg | Acton, Gary D | 25 mT AF demagnetization, (Dec025) | |
20 | NRM, Inclination after demagnetization | Incl (AF) | deg | Acton, Gary D | 25 mT AF demagnetization, (Inc025) | |
21 | NRM, Intensity | Inten (NRM) | mA/m | Acton, Gary D | NRM magnetization with 25 mT AF demagnetization (Int025) | |
22 | Natural remanent magnetization | NRM | mT | Acton, Gary D | 30 mT AF demagnetization, (AFD030) | |
23 | NRM, Declination after demagnetization | Decl (AF) | deg | Acton, Gary D | 30 mT AF demagnetization, (Dec030) | |
24 | NRM, Inclination after demagnetization | Incl (AF) | deg | Acton, Gary D | 30 mT AF demagnetization, (Inc030) | |
25 | NRM, Intensity | Inten (NRM) | mA/m | Acton, Gary D | NRM magnetization with 30 mT AF demagnetization (Int030) | |
26 | Natural remanent magnetization | NRM | mT | Acton, Gary D | 40 mT AF demagnetization, (AFD040) | |
27 | NRM, Declination after demagnetization | Decl (AF) | deg | Acton, Gary D | 40 mT AF demagnetization, (Dec040) | |
28 | NRM, Inclination after demagnetization | Incl (AF) | deg | Acton, Gary D | 40 mT AF demagnetization, (Inc040) | |
29 | NRM, Intensity | Inten (NRM) | mA/m | Acton, Gary D | NRM magnetization with 40 mT AF demagnetization (Int040) | |
30 | Natural remanent magnetization | NRM | mT | Acton, Gary D | 50 mT AF demagnetization, (AFD050) | |
31 | NRM, Declination after demagnetization | Decl (AF) | deg | Acton, Gary D | 50 mT AF demagnetization, (Dec050) | |
32 | NRM, Inclination after demagnetization | Incl (AF) | deg | Acton, Gary D | 50 mT AF demagnetization, (Inc050) | |
33 | NRM, Intensity | Inten (NRM) | mA/m | Acton, Gary D | NRM magnetization with 50 mT AF demagnetization (Int050) | |
34 | Natural remanent magnetization | NRM | mT | Acton, Gary D | 60 mT AF demagnetization, (AFD060) | |
35 | NRM, Declination after demagnetization | Decl (AF) | deg | Acton, Gary D | 60 mT AF demagnetization, (Dec060) | |
36 | NRM, Inclination after demagnetization | Incl (AF) | deg | Acton, Gary D | 60 mT AF demagnetization, (Inc060) | |
37 | NRM, Intensity | Inten (NRM) | mA/m | Acton, Gary D | NRM magnetization with 60 mT AF demagnetization (Int060) | |
38 | Natural remanent magnetization | NRM | mT | Acton, Gary D | 80 mT AF demagnetization, (AFD080) | |
39 | NRM, Declination after demagnetization | Decl (AF) | deg | Acton, Gary D | 80 mT AF demagnetization, (Dec080) | |
40 | NRM, Inclination after demagnetization | Incl (AF) | deg | Acton, Gary D | 80 mT AF demagnetization, (Inc080) | |
41 | NRM, Intensity | Inten (NRM) | mA/m | Acton, Gary D | NRM magnetization with 80 mT AF demagnetization (Int080) | |
42 | Inclination | Incl | deg | Acton, Gary D | Principal component analyses (PCA) | free-fitting option |
43 | Declination | Decl | deg | Acton, Gary D | Principal component analyses (PCA) | free-fitting option |
44 | Maximum angular deviation | MAD | deg | Acton, Gary D | Principal component analyses (PCA) | free-fitting option |
45 | Length of principal axis | Length | mA/m | Acton, Gary D | Principal component analyses (PCA) | free-fitting option |
46 | Deviation angle | Deviation | deg | Acton, Gary D | Principal component analyses (PCA) | deviation of best-fitting line from origin, free-fitting option |
47 | Number of steps | N steps | # | Acton, Gary D | Principal component analyses (PCA) | number of demagnetization steps used to fit the PCA line, free-fitting option |
48 | Demagnetization step | Demag step | mT | Acton, Gary D | Principal component analyses (PCA) | lowest demagnetization step used, free-fitting option |
49 | Demagnetization step | Demag step | mT | Acton, Gary D | Principal component analyses (PCA) | highest demagnetization step used, free-fitting option |
50 | Inclination | Incl | deg | Acton, Gary D | Principal component analyses (PCA) | line anchored to origin |
51 | Declination | Decl | deg | Acton, Gary D | Principal component analyses (PCA) | line anchored to origin |
52 | Maximum angular deviation | MAD | deg | Acton, Gary D | Principal component analyses (PCA) | line anchored to origin |
53 | Length of principal axis | Length | mA/m | Acton, Gary D | Principal component analyses (PCA) | line anchored to origin |
54 | Deviation angle | Deviation | deg | Acton, Gary D | Principal component analyses (PCA) | deviation of best-fitting line from origin, line anchored to origin |
55 | Number of steps | N steps | # | Acton, Gary D | Principal component analyses (PCA) | number of demagnetization steps used to fit the PCA line anchored to origin |
56 | Demagnetization step | Demag step | mT | Acton, Gary D | lowest demagnetization step used, line anchored to origin | |
57 | Demagnetization step | Demag step | mT | Acton, Gary D | highest demagnetization step used, line anchored to origin | |
58 | Inclination | Incl | deg | Acton, Gary D | stable end point (SEP) inclination, a Fisherian mean | |
59 | Declination | Decl | deg | Acton, Gary D | stable end point (SEP) declination, a Fisherian mean | |
60 | Precision parameter | k | Acton, Gary D | Fisherian precision parameter for SEP | ||
61 | Number of steps | N steps | # | Acton, Gary D | number of demagnetization steps used for SEP | |
62 | Angular distance | Angular dist | deg | Acton, Gary D | between PCA direction (free-fitting) and SEP direction | |
63 | Declination | Decl | deg | Acton, Gary D | mean declination for a drill core | |
64 | Declination | Decl | deg | Acton, Gary D | reorientation correction dependent on half from which sample was collected | |
65 | Declination | Decl | deg | Acton, Gary D | other reorientation correction related to sample handling | |
66 | Declination | Decl | deg | Acton, Gary D | sum of several reorientation corrections | |
67 | Declination | Decl | deg | Acton, Gary D | reoriented to approximate mean geographical coordinate | |
68 | Declination | Decl | deg | Acton, Gary D | correction for within-core rotation that occurs as core is collected | |
69 | Declination | Decl | deg | Acton, Gary D | preferred after all corrections have been applied | |
70 | Polarity | Polarity | Acton, Gary D | geomagnetic polarity (R=Reversed, N=Normal, T=Transitional, X=Uncertain) | ||
71 | Chronozone | Chronozone | Acton, Gary D | polarity chron age of sample |
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