Scientific Investigations Report 2009–5073
Table 6. Stable isotopes of oxygen and carbon in rock sample of Pole Canyon Limestone and ratio of strontium isotopes and concentration of strontium in rock samples of Pole Canyon Limestone, Tertiary granite, and Prospect Mountain Quartzite near Cave Springs at Great Basin National Park, Nevada. [Site locations are shown in figure 2. All rock samples were collected on September 8, 2007, between 7:45 and 9:30 AM Pacific Standard Time. Analyses were done by U.S. Geological Survey Yucca Mountain Project Environmental laboratory, Lakewood, Colorado. Symbol: –, not determined]
1 Ratio reported in delta (δ) notation as parts per thousand (permil). Delta is the relative difference between ratios of oxygen-18 to oxygen-16 (18O/16O) in sample of Pole Canyon Limestone to that in Vienna Standard Mean Ocean Water (VSMOW; Gonfiantini, 1978). A positive value represents a sample with more 18O relative to 16O than VSMOW. Standard error at 95-percent confidence level is 0.2 permil. 2 Ratios reported in delta (δ) notation as parts per thousand (permil). Delta is the relative difference between the ratios of oxygen-18 to oxygen-16 (18O/16O) and carbon-13 to carbon-12 (13C/ 12C) in sample of Pole Canyon Limestone to the respective ratio in a sample of belemnite from the Pee Dee Formation of South Carolina (PDB; Craig, 1957). Negative values of δ18O and δ13C represent samples with less 18O and 13C relative to 16O and 13C in the standard sample of PDB, respectively. Standard error at 95-percent confidence level is 0.2 permil for δ18O and 0.5 permil for δ13C. 3 Ratios are based on repetitive analyses on the seawater standard, EN-1. The error on the ratio of strontium-87 to strontium-86 (87Sr/86Sr) is ± 0.00005 at the 95-percent confidence level. |
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