Sager, William W (2004): (Table T4) Paleomagnetic properties of igneous samples from DSDP Site 92-597 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.779533, In supplement to: Sager, WW (2004): Data report: Paleomagnetism of basaltic rocks cored from western Pacific DSDP and ODP boreholes. In: Sager, WW; Kanazawa, T; Escutia, C (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 191, 1-27, https://doi.org/10.2973/odp.proc.sr.191.003.2004
Always quote citation above when using data! You can download the citation in several formats below.
Related to:
Nishitani, T (1986): Magnetic properties of basalt samples from Deep Sea Drilling Project Holes 597B and 597C. In: Leinen, M; Rea DK; et al. (eds.), Initial Reports of the Deep Sea Drilling Project, Washington (U.S. Govt. Printing Office), 92, 527-535, https://doi.org/10.2973/dsdp.proc.92.134.1986
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: -18.807200 * Longitude: -129.770300
Date/Time Start: 1983-03-02T00:00:00 * Date/Time End: 1983-03-02T00:00:00
Minimum DEPTH, sediment/rock: 54.49 m * Maximum DEPTH, sediment/rock: 132.67 m
Event(s):
92-597B * Latitude: -18.807200 * Longitude: -129.770300 * Date/Time: 1983-03-02T00:00:00 * Elevation: -4163.0 m * Penetration: 72.6 m * Recovery: 5.4 m * Location: South Pacific Ocean * Campaign: Leg92 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 2 cores; 18.2 m cored; 6.4 m drilled; 29.8 % recovery
92-597C * Latitude: -18.807200 * Longitude: -129.770300 * Date/Time: 1983-03-02T00:00:00 * Elevation: -4164.0 m * Penetration: 143.5 m * Recovery: 55.2 m * Location: South Pacific Ocean * Campaign: Leg92 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 11 cores; 97 m cored; 3 m drilled; 56.9 % recovery
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Event label | Event | ||||
| 2 | Sample code/label | Sample label | Sager, William W | DSDP/ODP/IODP sample designation | ||
| 3 | Author(s) | Author(s) | Sager, William W | |||
| 4 | DEPTH, sediment/rock | Depth sed | m | Geocode – mbsf | ||
| 5 | NRM, Intensity | Inten (NRM) | mA/m | Sager, William W | ||
| 6 | ChRM, Inclination | Incl (ChRM) | deg | Sager, William W | Principal component analyses (PCA) | empty fields = inclination unstable |
| 7 | Demag Type | Demag Type | Sager, William W | A = alternating field | ||
| 8 | Sample amount, subset | N subset | # | Sager, William W | number of measurements used for PCA | |
| 9 | Demagnetization level | Level | mT | Sager, William W | lower | |
| 10 | Demagnetization level | Level | mT | Sager, William W | upper | |
| 11 | Maximum angular deviation | MAD | deg | Sager, William W | ||
| 12 | Colatitude | Colat | deg | Sager, William W | ||
| 13 | Sample ID | Sample ID | Sager, William W | group number | ||
| 14 | Sample comment | Sample comment | Sager, William W |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
1568 data points
Data
| 1 Event | 2 Sample label (DSDP/ODP/IODP sample designation) | 3 Author(s) | 4 Depth sed [m] (mbsf) | 5 Inten (NRM) [mA/m] | 6 Incl (ChRM) [deg] (empty fields = inclination un...) | 7 Demag Type (A = alternating field) | 8 N subset [#] (number of measurements used f...) | 9 Level [mT] (lower) | 10 Level [mT] (upper) | 11 MAD [deg] | 12 Colat [deg] | 13 Sample ID (group number) | 14 Sample comment |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 92-597B | 92-597B-2R-1,20 | Nishitani (1986) | 54.49 | 2800 | 53.3 | A | 56.1 | 1 | |||||
| 92-597B | 92-597B-2R-1,28 | this study | 54.57 | 1400 | 35.0 | A | 4 | 20 | 30 | 7.4 | 70.7 | 1 | |
| 92-597B | 92-597B-2R-1,80 | this study | 55.17 | 1100 | 49.2 | A | 4 | 15 | 28 | 1.9 | 59.9 | 1 | |
| 92-597B | 92-597B-2R-1,91 | this study | 55.88 | 500 | 40.1 | A | 4 | 20 | 30 | 12.3 | 67.2 | 1 | |
| 92-597B | 92-597B-2R-1,95 | Nishitani (1986) | 55.24 | 2700 | 53.6 | A | 55.9 | 1 | |||||
| 92-597B | 92-597B-2R-2,7 | this study | 55.96 | 3500 | 53.0 | A | 4 | 10 | 25 | 0.8 | 56.4 | 1 | |
| 92-597B | 92-597B-2R-2,48 | Nishitani (1986) | 56.37 | 2000 | 41.0 | A | 66.5 | 1 | |||||
| 92-597B | 92-597B-2R-2,68 | this study | 56.57 | 1700 | 37.6 | A | 5 | 10 | 28 | 1.5 | 68.9 | 1 | |
| 92-597B | 92-597B-2R-2,100 | this study | 56.89 | 600 | 40.5 | A | 4 | 10 | 25 | 3.0 | 66.9 | 1 | |
| 92-597B | 92-597B-2R-2,110 | Nishitani (1986) | 57.02 | 3300 | 44.1 | A | 64.1 | 1 | |||||
| 92-597B | 92-597B-2R-2,131 | Nishitani (1986) | 57.23 | 2500 | 46.1 | A | 62.5 | 1 | |||||
| 92-597B | 92-597B-2R-3,29 | Nishitani (1986) | 57.71 | 2500 | 46.9 | A | 61.9 | 1 | |||||
| 92-597B | 92-597B-2R-3,74 | this study | 58.16 | 1100 | 47.3 | A | 3 | 10 | 25 | 2.8 | 61.5 | 1 | |
| 92-597B | 92-597B-2R-3,86 | this study | 58.28 | 1400 | 47.1 | A | 4 | 10 | 25 | 3.8 | 61.7 | 1 | |
| 92-597B | 92-597B-2R-3,106 | this study | 58.48 | 900 | 38.5 | A | 4 | 5 | 20 | 7.5 | 68.3 | 1 | |
| 92-597B | 92-597B-2R-3,113 | Nishitani (1986) | 58.56 | 4400 | 57.4 | A | 52.0 | 1 | |||||
| 92-597B | 92-597B-3R-1,3 | Nishitani (1986) | 63.55 | 2300 | 44.7 | A | 63.7 | 1 | |||||
| 92-597B | 92-597B-3R-1,29 | this study | 63.81 | 1700 | 41.0 | A | 4 | 10 | 25 | 2.8 | 66.5 | 1 | |
| 92-597B | 92-597B-3R-1,51 | this study | 64.03 | 900 | 38.9 | A | 4 | 10 | 25 | 2.9 | 68.0 | 1 | |
| 92-597B | 92-597B-3R-1,97 | this study | 64.49 | 1800 | 39.1 | A | 4 | 10 | 25 | 2.1 | 67.9 | 1 | |
| 92-597B | 92-597B-3R-1,119 | this study | 64.71 | 700 | 38.3 | A | 4 | 10 | 25 | 4.3 | 68.5 | 1 | |
| 92-597B | 92-597B-3R-1,132 | Nishitani (1986) | 64.84 | 2700 | 40.5 | A | 66.9 | 1 | |||||
| 92-597B | 92-597B-3R-2,14 | this study | 65.16 | 800 | 51.9 | A | 4 | 10 | 25 | 1.5 | 57.5 | 1 | |
| 92-597B | 92-597B-3R-2,23 | Nishitani (1986) | 65.25 | 2200 | 35.3 | A | 70.5 | 1 | |||||
| 92-597B | 92-597B-3R-2,26 | Nishitani (1986) | 65.42 | 2500 | 36.7 | A | 69.6 | 1 | |||||
| 92-597C | 92-597C-3R-1,18 | this study | 55.67 | 3000 | 37.4 | A | 4 | 10 | 25 | 0.7 | 69.1 | 1 | |
| 92-597C | 92-597C-3R-1,24 | Nishitani (1986) | 55.73 | 2800 | 45.7 | A | 62.9 | 1 | |||||
| 92-597C | 92-597C-3R-1,48 | this study | 55.97 | 600 | 32.3 | A | 4 | 10 | 25 | 5.6 | 72.5 | 1 | |
| 92-597C | 92-597C-3R-1,78 | this study | 56.27 | 600 | A | 1 | |||||||
| 92-597C | 92-597C-3R-1,104 | this study | 56.53 | 800 | 47.7 | A | 3 | 10 | 20 | 4.2 | 61.2 | 1 | |
| 92-597C | 92-597C-3R-1,134 | Nishitani (1986) | 56.83 | 3100 | 50.1 | A | 59.1 | 1 | |||||
| 92-597C | 92-597C-3R-2,13 | this study | 57.12 | 900 | A | 1 | |||||||
| 92-597C | 92-597C-3R-2,43 | Nishitani (1986) | 57.42 | 2400 | 36.5 | A | 69.7 | 1 | |||||
| 92-597C | 92-597C-3R-2,81 | this study | 57.80 | 1100 | 45.4 | A | 4 | 10 | 25 | 2.8 | 63.1 | 1 | |
| 92-597C | 92-597C-3R-2,123 | this study | 58.22 | 1600 | 33.6 | A | 4 | 10 | 25 | 2.5 | 71.6 | 1 | |
| 92-597C | 92-597C-3R-2,146 | this study | 58.45 | 2600 | A | 1 | |||||||
| 92-597C | 92-597C-3R-3,5 | Nishitani (1986) | 58.57 | 2700 | 60.1 | A | 49.0 | 1 | datum not used in average colatitude calculations | ||||
| 92-597C | 92-597C-3R-3,38 | this study | 58.90 | 2500 | 32.4 | A | 4 | 10 | 25 | 0.4 | 1 | ||
| 92-597C | 92-597C-3R-3,52 | Nishitani (1986) | 59.04 | 2500 | 31.2 | A | 73.2 | 1 | |||||
| 92-597C | 92-597C-3R-3,71 | this study | 59.23 | 4200 | 43.1 | A | 4 | 10 | 25 | 1.5 | 64.9 | 1 | |
| 92-597C | 92-597C-4R-1,55 | this study | 65.07 | 1900 | A | 1 | |||||||
| 92-597C | 92-597C-4R-1,60 | Nishitani (1986) | 65.12 | 4100 | 37.9 | A | 68.7 | 1 | |||||
| 92-597C | 92-597C-4R-1,70 | this study | 65.22 | 600 | -58.4 | A | 4 | 15 | 28 | 2.4 | 50.9 | 1 | inclination: sample assumed to be inverted |
| 92-597C | 92-597C-4R-1,120 | Nishitani (1986) | 65.72 | 3300 | 41.3 | A | 66.3 | 1 | |||||
| 92-597C | 92-597C-4R-2,21 | Nishitani (1986) | 66.72 | 3100 | 48.2 | A | 60.8 | 1 | |||||
| 92-597C | 92-597C-4R-2,55 | this study | 67.06 | 1100 | 61.7 | A | 3 | 10 | 20 | 4.3 | 47.1 | 2 | |
| 92-597C | 92-597C-4R-2,87 | this study | 67.38 | 2300 | -63.3 | A | 3 | 28 | 35 | 3.4 | 45.2 | 2 | inclination: sample assumed to be inverted |
| 92-597C | 92-597C-4R-2,109 | this study | 67.60 | 1800 | A | 2 | |||||||
| 92-597C | 92-597C-4R-2,111 | Nishitani (1986) | 67.13 | 2900 | 55.8 | A | 53.7 | 2 | |||||
| 92-597C | 92-597C-4R-3,27 | Nishitani (1986) | 67.79 | 3300 | 60.4 | A | 48.6 | 2 | |||||
| 92-597C | 92-597C-4R-3,49 | this study | 68.01 | 3700 | A | 2 | |||||||
| 92-597C | 92-597C-4R-3,91 | Nishitani (1986) | 68.43 | 2700 | 61.0 | A | 47.9 | 2 | |||||
| 92-597C | 92-597C-4R-3,139 | this study | 68.91 | 2200 | A | 3 | |||||||
| 92-597C | 92-597C-4R-4,23 | Nishitani (1986) | 69.25 | 2700 | 44.9 | A | 63.5 | 3 | |||||
| 92-597C | 92-597C-4R-4,62 | this study | 69.64 | 5100 | 53.5 | A | 3 | 10 | 20 | 2.9 | 56.0 | 3 | |
| 92-597C | 92-597C-4R-4,76 | Nishitani (1986) | 69.78 | 3300 | 48.5 | A | 60.5 | 3 | |||||
| 92-597C | 92-597C-4R-4,127 | this study | 70.29 | 2000 | A | 3 | |||||||
| 92-597C | 92-597C-4R-5,23 | this study | 70.75 | 2600 | A | 3 | |||||||
| 92-597C | 92-597C-4R-5,26 | Nishitani (1986) | 70.78 | 2300 | 45.3 | A | 63.2 | 3 | |||||
| 92-597C | 92-597C-4R-5,71 | Nishitani (1986) | 71.22 | 2300 | 45.6 | A | 63.0 | 3 | |||||
| 92-597C | 92-597C-4R-5,89 | this study | 71.41 | 1000 | A | 3 | |||||||
| 92-597C | 92-597C-4R-5,118 | this study | 71.70 | 2200 | A | 3 | |||||||
| 92-597C | 92-597C-4R-6,21 | Nishitani (1986) | 72.22 | 2300 | 65.7 | A | 42.1 | 3 | datum not used in average colatitude calculations | ||||
| 92-597C | 92-597C-4R-6,42 | this study | 72.43 | 1300 | A | 3 | |||||||
| 92-597C | 92-597C-4R-6,73 | Nishitani (1986) | 72.75 | 2000 | 43.0 | A | 65.0 | 3 | |||||
| 92-597C | 92-597C-4R-6,100 | this study | 73.01 | 2200 | 53.0 | A | 4 | 10 | 25 | 1.5 | 56.4 | 3 | |
| 92-597C | 92-597C-5R-1,9 | this study | 73.61 | 1200 | A | 3 | |||||||
| 92-597C | 92-597C-5R-1,62 | this study | 74.14 | 7300 | 52.2 | A | 3 | 10 | 20 | 2.2 | 57.2 | 3 | |
| 92-597C | 92-597C-5R-1,129 | Nishitani (1986) | 74.81 | 2600 | 41.0 | A | 66.5 | 3 | |||||
| 92-597C | 92-597C-5R-1,134 | this study | 74.86 | 1200 | 41.2 | A | 3 | 10 | 20 | 3.0 | 66.4 | 3 | |
| 92-597C | 92-597C-5R-2,63 | Nishitani (1986) | 75.64 | 4000 | 46.1 | A | 62.5 | 3 | |||||
| 92-597C | 92-597C-6R-1,28 | this study | 82.80 | 2300 | A | 4 | |||||||
| 92-597C | 92-597C-6R-1,109 | Nishitani (1986) | 83.61 | 3600 | 50.6 | A | 58.7 | 4 | |||||
| 92-597C | 92-597C-6R-1,119 | this study | 83.71 | 4600 | 56.4 | A | 3 | 10 | 20 | 0.4 | 53.0 | 4 | |
| 92-597C | 92-597C-6R-2,12 | this study | 84.14 | 1500 | -34.6 | A | 3 | 10 | 20 | 1.8 | 71.0 | 4 | inclination: sample assumed to be inverted; datum not used in average colatitude calculations |
| 92-597C | 92-597C-6R-2,35 | this study | 84.37 | 1300 | 47.4 | A | 4 | 10 | 25 | 4.5 | 61.5 | 4 | |
| 92-597C | 92-597C-6R-2,49 | Nishitani (1986) | 84.51 | 2300 | 46.5 | A | 62.2 | 4 | |||||
| 92-597C | 92-597C-6R-3,62 | Nishitani (1986) | 86.14 | 2900 | 49.3 | A | 59.8 | 4 | |||||
| 92-597C | 92-597C-6R-3,55 | this study | 86.07 | 2100 | A | 4 | |||||||
| 92-597C | 92-597C-6R-3,78 | this study | 86.30 | 1000 | A | 4 | |||||||
| 92-597C | 92-597C-6R-3,105 | Nishitani (1986) | 86.57 | 700 | 49.2 | A | 4 | 25 | 35 | 2.1 | 4 | ||
| 92-597C | 92-597C-6R-4,19 | this study | 87.21 | 2400 | 54.6 | A | 4 | 10 | 25 | 3.6 | 54.9 | 4 | |
| 92-597C | 92-597C-6R-4,53 | this study | 87.55 | 1700 | A | 5 | |||||||
| 92-597C | 92-597C-6R-4,74 | Nishitani (1986) | 87.76 | 3000 | 37.8 | A | 68.8 | 5 | |||||
| 92-597C | 92-597C-6R-4,116 | this study | 88.18 | 2100 | A | 5 | |||||||
| 92-597C | 92-597C-6R-5,38 | this study | 88.90 | 600 | 27.5 | A | 3 | 10 | 20 | 3.5 | 75.4 | 5 | |
| 92-597C | 92-597C-6R-5,58 | Nishitani (1986) | 89.10 | 3300 | 37.9 | A | 68.7 | 5 | |||||
| 92-597C | 92-597C-6R-5,82 | this study | 89.34 | 2300 | A | 5 | |||||||
| 92-597C | 92-597C-7R-1,70 | this study | 92.22 | 1800 | 31.0 | A | 4 | 15 | 28 | 2.2 | 73.3 | 5 | |
| 92-597C | 92-597C-7R-1,128 | this study | 92.80 | 5800 | 48.1 | A | 4 | 10 | 25 | 1.6 | 60.9 | 6 | |
| 92-597C | 92-597C-7R-1,115 | Nishitani (1986) | 92.67 | 3100 | 50.2 | A | 59.0 | 6 | |||||
| 92-597C | 92-597C-7R-2,7 | this study | 93.08 | 2800 | A | 6 | |||||||
| 92-597C | 92-597C-7R-2,16 | Nishitani (1986) | 93.17 | 3300 | 45.6 | A | 63.0 | 6 | |||||
| 92-597C | 92-597C-7R-2,66 | this study | 93.67 | 6700 | 49.8 | A | 4 | 15 | 20 | 2.4 | 59.4 | 6 | |
| 92-597C | 92-597C-7R-2,117 | Nishitani (1986) | 94.18 | 3700 | 50.6 | A | 58.7 | 6 | |||||
| 92-597C | 92-597C-7R-2,123 | this study | 94.24 | 3900 | 47.4 | A | 4 | 10 | 25 | 0.5 | 61.5 | 6 | |
| 92-597C | 92-597C-7R-3,10 | this study | 94.61 | 4300 | 55.2 | A | 4 | 10 | 25 | 0.7 | 54.3 | 6 | |
| 92-597C | 92-597C-7R-4,17 | this study | 96.19 | 5200 | 58.9 | A | 4 | 10 | 25 | 2.5 | 50.3 | 6 | |
| 92-597C | 92-597C-7R-4,18 | Nishitani (1986) | 96.20 | 3000 | 54.0 | A | 55.5 | 6 | |||||
| 92-597C | 92-597C-7R-4,87 | Nishitani (1986) | 96.89 | 4400 | 50.2 | A | 59.0 | 6 | |||||
| 92-597C | 92-597C-7R-4,91 | this study | 96.93 | 6700 | -49.9 | A | 4 | 28 | 35 | 2.2 | 59.3 | 6 | inclination: sample assumed to be inverted |
| 92-597C | 92-597C-7R-4,111 | Nishitani (1986) | 97.13 | 2800 | 56.0 | A | 53.5 | 6 | |||||
| 92-597C | 92-597C-7R-4,137 | Nishitani (1986) | 97.39 | 1900 | -41.1 | A | 66.4 | 6 | inclination: sample assumed to be inverted | ||||
| 92-597C | 92-597C-7R-4,141 | this study | 97.43 | 2300 | -65.6 | A | 4 | 5 | 20 | 1.2 | 42.2 | 6 | inclination: sample assumed to be inverted; datum not used in average colatitude calculations |
| 92-597C | 92-597C-7R-5,70 | Nishitani (1986) | 98.22 | 2200 | -76.7 | A | 25.3 | 6 | inclination: sample assumed to be inverted; datum not used in average colatitude calculations | ||||
| 92-597C | 92-597C-8R-1,9 | Nishitani (1986) | 100.60 | 3200 | 41.9 | A | 65.8 | 7 | |||||
| 92-597C | 92-597C-8R-1,25 | this study | 100.76 | 1800 | 39.6 | A | 4 | 10 | 25 | 2.0 | 67.5 | 7 | |
| 92-597C | 92-597C-8R-1,94 | Nishitani (1986) | 101.46 | 3200 | 41.0 | A | 66.5 | 7 | |||||
| 92-597C | 92-597C-8R-1,103 | this study | 101.54 | 3700 | 40.4 | A | 4 | 15 | 28 | 1.2 | 66.9 | 7 | |
| 92-597C | 92-597C-8R-2,41 | this study | 102.42 | 3500 | 41.0 | A | 4 | 10 | 25 | 1.9 | 66.5 | 7 | |
| 92-597C | 92-597C-8R-2,50 | Nishitani (1986) | 102.51 | 2800 | 39.1 | A | 67.9 | 7 | |||||
| 92-597C | 92-597C-8R-2,66 | this study | 102.67 | 2200 | 41.3 | A | 3 | 10 | 20 | 2.3 | 66.3 | 7 | |
| 92-597C | 92-597C-8R-2,137 | this study | 103.38 | 2700 | 46.1 | A | 4 | 15 | 28 | 1.5 | 62.5 | 7 | |
| 92-597C | 92-597C-8R-3,5 | Nishitani (1986) | 103.57 | 2500 | 36.5 | A | 69.7 | 7 | |||||
| 92-597C | 92-597C-8R-3,44 | this study | 103.96 | 1500 | A | 7 | |||||||
| 92-597C | 92-597C-8R-3,130 | Nishitani (1986) | 104.82 | 2500 | 22.1 | A | 78.5 | 7 | datum not used in average colatitude calculations | ||||
| 92-597C | 92-597C-8R-3,138 | this study | 104.90 | 2400 | 30.8 | A | 5 | 10 | 28 | 2.6 | 73.4 | 7 | |
| 92-597C | 92-597C-8R-4,70 | this study | 105.72 | 1800 | 31.7 | A | 4 | 10 | 25 | 4.9 | 72.8 | 7 | |
| 92-597C | 92-597C-8R-4,102 | Nishitani (1986) | 106.04 | 2600 | 40.2 | A | 67.1 | 7 | |||||
| 92-597C | 92-597C-8R-4,103 | this study | 106.05 | 2900 | 43.5 | A | 4 | 15 | 28 | 1.7 | 64.6 | 7 | |
| 92-597C | 92-597C-8R-4,137 | this study | 106.39 | 1000 | 33.1 | A | 3 | 20 | 28 | 2.3 | 71.9 | 7 | |
| 92-597C | 92-597C-8R-5,49 | Nishitani (1986) | 107.01 | 3900 | 34.8 | A | 4 | 10 | 25 | 0.3 | 70.8 | 7 | |
| 92-597C | 92-597C-8R-5,60 | Nishitani (1986) | 107.12 | 2700 | 37.0 | A | 69.4 | 7 | |||||
| 92-597C | 92-597C-8R-5,88 | this study | 107.40 | 2500 | A | 7 | |||||||
| 92-597C | 92-597C-8R-6,30 | this study | 108.32 | 1300 | 32.1 | A | 4 | 10 | 25 | 2.7 | 72.6 | 7 | |
| 92-597C | 92-597C-8R-6,56 | Nishitani (1986) | 108.58 | 3300 | 40.9 | A | 66.6 | 7 | |||||
| 92-597C | 92-597C-8R-6,92 | this study | 108.94 | 1200 | -22.7 | A | 3 | 20 | 28 | 0.7 | 78.2 | 7 | inclination: sample assumed to be inverted; datum not used in average colatitude calculations |
| 92-597C | 92-597C-8R-6,135 | this study | 109.37 | 2700 | 37.2 | A | 4 | 10 | 25 | 3.7 | 69.2 | 7 | |
| 92-597C | 92-597C-8R-7,7 | this study | 109.57 | 1400 | 41.6 | A | 3 | 15 | 25 | 1.9 | 66.1 | 7 | |
| 92-597C | 92-597C-8R-7,9 | Nishitani (1986) | 109.59 | 2900 | 44.0 | A | 64.2 | 7 | |||||
| 92-597C | 92-597C-8R-7,86 | this study | 110.36 | 2000 | 28.9 | A | 4 | 10 | 25 | 6.3 | 74.6 | 7 | |
| 92-597C | 92-597C-9R-1,9 | Nishitani (1986) | 109.59 | 3800 | 36.5 | A | 69.7 | 7 | |||||
| 92-597C | 92-597C-9R-1,76 | this study | 110.27 | 800 | A | 7 | |||||||
| 92-597C | 92-597C-9R-1,139 | Nishitani (1986) | 110.90 | 2200 | 34.5 | A | 4 | 15 | 28 | 1.7 | 7 | ||
| 92-597C | 92-597C-9R-1,141 | this study | 110.92 | 1400 | A | 7 | |||||||
| 92-597C | 92-597C-9R-1,142 | Nishitani (1986) | 110.93 | 3200 | 38.9 | A | 68.0 | 7 | |||||
| 92-597C | 92-597C-9R-2,15 | this study | 111.17 | 2800 | 60.8 | A | 4 | 20 | 35 | 1.4 | 48.2 | 7 | datum not used in average colatitude calculations |
| 92-597C | 92-597C-9R-2,60 | this study | 111.62 | 3300 | -46.6 | A | 5 | 30 | 45 | 0.4 | 62.1 | 7 | inclination: sample assumed to be inverted |
| 92-597C | 92-597C-9R-2,70 | Nishitani (1986) | 111.72 | 3400 | 41.6 | A | 66.1 | 7 | |||||
| 92-597C | 92-597C-9R-3,82 | this study | 113.33 | 1100 | -60.6 | A | 7 | 28 | 45 | 5.7 | 48.4 | 7 | inclination: sample assumed to be inverted; datum not used in average colatitude calculations |
| 92-597C | 92-597C-9R-3,88 | Nishitani (1986) | 113.39 | 2900 | 47.3 | A | 61.5 | 7 | |||||
| 92-597C | 92-597C-9R-3,140 | this study | 113.91 | 900 | -51.3 | A | 4 | 20 | 30 | 5.1 | 58.0 | 7 | inclination: sample assumed to be inverted |
| 92-597C | 92-597C-9R-4,64 | this study | 114.66 | 600 | A | 7 | |||||||
| 92-597C | 92-597C-9R-4,103 | Nishitani (1986) | 115.05 | 3100 | 41.9 | A | 65.8 | 7 | |||||
| 92-597C | 92-597C-9R-4,104 | this study | 115.06 | 4600 | 33.9 | A | 4 | 20 | 30 | 6.2 | 71.4 | 7 | |
| 92-597C | 92-597C-10R-1,74 | this study | 119.26 | 6500 | 43.4 | A | 4 | 15 | 25 | 2.0 | 64.7 | 8 | |
| 92-597C | 92-597C-10R-1,112 | Nishitani (1986) | 119.64 | 2900 | 40.1 | A | 67.2 | 8 | |||||
| 92-597C | 92-597C-10R-1,128 | this study | 119.80 | 2900 | 37.5 | A | 4 | 10 | 25 | 2.2 | 69.0 | 8 | |
| 92-597C | 92-597C-10R-2,39 | this study | 120.41 | 2500 | 44.5 | A | 4 | 10 | 25 | 0.6 | 63.8 | 8 | |
| 92-597C | 92-597C-10R-2,86 | this study | 120.88 | 1900 | 52.9 | A | 4 | 10 | 25 | 3.3 | 56.5 | 8 | |
| 92-597C | 92-597C-10R-2,104 | Nishitani (1986) | 121.06 | 1900 | 43.6 | A | 64.5 | 8 | |||||
| 92-597C | 92-597C-10R-3,33 | this study | 121.85 | 900 | A | 8 | |||||||
| 92-597C | 92-597C-10R-3,72 | this study | 122.24 | 2100 | 42.7 | A | 4 | 20 | 35 | 1.1 | 65.2 | 8 | |
| 92-597C | 92-597C-10R-3,94 | Nishitani (1986) | 122.46 | 2000 | 43.9 | A | 64.3 | 8 | |||||
| 92-597C | 92-597C-10R-3,115 | this study | 122.67 | 2200 | 31.8 | A | 4 | 10 | 25 | 4.3 | 72.8 | 8 | |
| 92-597C | 92-597C-10R-4,46 | this study | 123.48 | 1000 | 39.6 | A | 4 | 10 | 25 | 2.9 | 67.5 | 8 | |
| 92-597C | 92-597C-10R-4,91 | Nishitani (1986) | 123.93 | 1500 | 52.6 | A | 56.8 | 8 | |||||
| 92-597C | 92-597C-10R-4,133 | this study | 124.35 | 1100 | 32.8 | A | 3 | 10 | 20 | 4.6 | 72.1 | 8 | |
| 92-597C | 92-597C-10R-5,52 | this study | 125.02 | 1000 | A | 8 | |||||||
| 92-597C | 92-597C-10R-5,84 | Nishitani (1986) | 125.36 | 1600 | 46.4 | A | 62.3 | 8 | |||||
| 92-597C | 92-597C-10R-5,112 | this study | 125.62 | 2100 | -49.5 | A | 4 | 15 | 28 | 0.2 | 59.7 | 8 | inclination: sample assumed to be inverted |
| 92-597C | 92-597C-10R-6,19 | this study | 126.21 | 500 | 46.1 | A | 4 | 20 | 30 | 2.6 | 62.5 | 8 | |
| 92-597C | 92-597C-10R-6,36 | Nishitani (1986) | 126.38 | 1700 | 40.5 | A | 66.9 | 8 | |||||
| 92-597C | 92-597C-10R-6,103 | this study | 127.05 | 900 | 44.8 | A | 4 | 20 | 30 | 1.6 | 63.6 | 8 | |
| 92-597C | 92-597C-10R-7,30 | this study | 127.31 | 1400 | 45.5 | A | 4 | 15 | 28 | 1.7 | 63.0 | 8 | |
| 92-597C | 92-597C-10R-7,42 | Nishitani (1986) | 127.93 | 1600 | 42.2 | A | 65.6 | 8 | |||||
| 92-597C | 92-597C-10R-7,84 | Nishitani (1986) | 127.85 | 1200 | 21.0 | A | 4 | 15 | 28 | 1.0 | 79.1 | 8 | datum not used in average colatitude calculations |
| 92-597C | 92-597C-11R-1,32 | this study | 127.84 | 700 | 63.8 | A | 4 | 20 | 30 | 0.6 | 44.5 | 8 | datum not used in average colatitude calculations |
| 92-597C | 92-597C-11R-1,79 | Nishitani (1986) | 128.31 | 1600 | 47.1 | A | 61.7 | 8 | |||||
| 92-597C | 92-597C-11R-1,116 | this study | 128.68 | 400 | 44.7 | A | 4 | 15 | 28 | 1.2 | 63.7 | 8 | |
| 92-597C | 92-597C-11R-2,46 | this study | 129.48 | 700 | A | 8 | |||||||
| 92-597C | 92-597C-11R-2,103 | Nishitani (1986) | 130.05 | 1600 | 43.8 | A | 64.4 | 8 | |||||
| 92-597C | 92-597C-11R-2,138 | this study | 130.40 | 700 | 48.1 | A | 4 | 25 | 40 | 0.4 | 60.9 | 8 | |
| 92-597C | 92-597C-11R-3,13 | Nishitani (1986) | 130.64 | 1700 | 45.6 | A | 63.0 | 8 | |||||
| 92-597C | 92-597C-11R-3,47 | this study | 130.98 | 1800 | 41.6 | A | 4 | 10 | 25 | 0.9 | 66.1 | 8 | |
| 92-597C | 92-597C-11R-3,93 | this study | 131.44 | 1200 | 40.4 | A | 4 | 15 | 28 | 0.9 | 66.9 | 8 | |
| 92-597C | 92-597C-11R-4,25 | this study | 132.26 | 900 | 23.2 | A | 4 | 10 | 25 | 3.3 | 77.9 | 8 | datum not used in average colatitude calculations |
| 92-597C | 92-597C-11R-4,39 | this study | 132.40 | 1400 | -45.2 | A | 4 | 25 | 32 | 1.2 | 63.3 | 8 | inclination: sample assumed to be inverted |
| 92-597C | 92-597C-11R-4,50 | this study | 132.51 | 1600 | 47.0 | A | 4 | 10 | 25 | 1.1 | 61.8 | 8 | |
| 92-597C | 92-597C-11R-4,62 | Nishitani (1986) | 132.63 | 1700 | 42.9 | A | 65.1 | 8 | |||||
| 92-597C | 92-597C-11R-4,66 | this study | 132.67 | 1600 | 32.2 | A | 4 | 10 | 25 | 0.5 | 72.5 | 8 |