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John, Barbara E; Foster, David A; Murphy, John M; Cheadle, Michael J; Baines, A Graham; Fanning, C Mark; Copeland, Peter (2004): (Table 3) Fission analsyse of minerals from ODP Hole 176-735B [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.714869, In supplement to: John, BE et al. (2004): Determining the cooling history of in situ lower oceanic crust-Atlantis Bank, SW Indian Ridge. Earth and Planetary Science Letters, 222(1), 145-160, https://doi.org/10.1016/j.epsl.2004.02.014

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Project(s):
Coverage:
Latitude: -32.723210 * Longitude: 57.266010
Date/Time Start: 1997-10-24T13:45:00 * Date/Time End: 1997-12-01T19:00:00
Minimum Elevation: -720.6 m * Maximum Elevation: -720.6 m
Event(s):
176-735B * Latitude: -32.723210 * Longitude: 57.266010 * Date/Time Start: 1997-10-24T13:45:00 * Date/Time End: 1997-12-01T19:00:00 * Elevation: -720.6 m * Penetration: 1508 m * Recovery: 865.99 m * Location: Indian Ocean * Campaign: Leg176 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 122 cores; 1003.2 m cored; 504.8 m drilled; 86.3 % recovery
Comment:
AGE is the track age. zeta=377 +/- 10 for zircon; 435.1 +/- 5 for sphene, 330 +/- 10 for apatite, kappa(d)=1.551*10**-10/year, g=0.5.
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1AGEAgeka BPGeocode
2Age, standard deviationAge std dev±John, Barbara E
3NumberNoJohn, Barbara E
4Mineral nameMineralJohn, Barbara E
5Grains, counted/analyzedGrains#John, Barbara E
6Fission-tracks, spontaneous, densityp s106 #/cm2John, Barbara E
7Number of observationsNOBS#John, Barbara ENumber of tracks ps
8Fission-tracks, induced, densityp i106 #/cm2John, Barbara E
9Number of observationsNOBS#John, Barbara ENumber of tracks pi
10Fission-tracks, density, counted in stanp d106 #/cm2John, Barbara Etrack density in muscovite detector covering CN-5 (10 ppm)
11Number of observationsNOBS#John, Barbara ENumber of tracks pd
12Probability, chi-square testChi-sqrJohn, Barbara Echi-squared probability
13UraniumUmg/kgJohn, Barbara E
Size:
156 data points

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