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Basak, Chandranath; Martin, Ellen E; Kamenov, George D (2011): (Table 6) Sr and Nd isotope duplicates of authigenic Fe-Mn phases of ODP Site 177-1090 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.780144, In supplement to: Basak, C et al. (2011): Seawater Pb isotopes extracted from Cenozoic marine sediments. Chemical Geology, 286(3-4), 94-108, https://doi.org/10.1016/j.chemgeo.2011.04.007

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Project(s):
Coverage:
Latitude: -42.913617 * Longitude: 8.899817
Date/Time Start: 1997-12-25T00:00:00 * Date/Time End: 1997-12-25T00:00:00
Minimum DEPTH, sediment/rock: 104.91 m * Maximum DEPTH, sediment/rock: 375.03 m
Event(s):
177-1090 * Latitude: -42.913617 * Longitude: 8.899817 * Date/Time: 1997-12-25T00:00:00 * Elevation: -3701.6 m * Penetration: 936.4 m * Recovery: 874.9 m * Location: South Atlantic Ocean * Campaign: Leg177 * Basis: Joides Resolution * Method/Device: Composite Core (COMPCORE) * Comment: 101 cores; 936.4 m cored; 0 m drilled; 93.4% recovery
Comment:
Sediment depth is given in mcd. Age model after Channell et al. (2003, datasets: doi:10.1594/PANGAEA.717737). Sr ratios were measured in a static mode and using time resolved analysis (TRA) on a Nu MC-ICPMS and 87Sr/86Sr ratios were corrected for mass-bias using an exponential law and 86Sr/88Sr=0.1194. The long-term average value of the TRA-measured 87Sr/86Sr of NBS 987 is 0.710246 (+/-0.000030, 2 sigma). All reported 143Nd/144Nd ratios were corrected for mass fractionation using 146Nd/144Nd=0.7219. International standard JNdi-1 was analyzed between every 5-6 unknown samples and the average of these standard runs were compared to a long term TIMS JNdi-1 value of 0.512103 to determine a correction factor for each of the samples analyzed on that day. Long term external reproducibility of JNdi-1 analyses on the Nu is 0.000014 (0.3 epsilon-Nd units).
Size:
40 data points

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