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Data Series 280

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Data Series 280

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Table 7. Selected trace element concentrations and strontium isotopic compositions (87Sr/86Sr) in core samples from boreholes UE‑25 a #3 and UE-25 p #1, Nevada Test Site, Nye County, Nevada.

[Siliciclastic lithologies for samples from surface to 697.2-m depth in borehole UE–25 a #3 consist of Mississippian (middle Chester to early Osage stages) Chainman Shale and Gap Wash Formation (Maldonado and others, 1979; Cole and Cashman, 1998). Underlying core is undifferentiated Devonian carbonate (Du). Stratigraphic units for borehole UE–25 p #1 are from Carr and others (1986). Stratigraphic unit symbols are defined in table 1. Analysis type: WR indicates that strontium isotopic compositions (87Sr/86Sr) were determined on whole-rock digestions using concentrated hydrofluoric, nitric, hydrochloric, and sulfuric acids; HCl–L indicates that 87Sr/86Sr values were determined on dilute hydrochloric acid leachates of powdered rock samples. Strontium isotopic compositions are given in delta notation (δ87Sr = [(87Sr/86Srsample/87Sr/86Srmsw)-1]×1,000 and δ87Srt = [(87Sr/86Srsample/87Sr/86Srpsw)-1]×1,000, where 87Sr/86Srmsw is the value for modern seawater and 87Sr/86Srpsw is the value for paleoseawater at the time of deposition). Abbreviations and symbols: Rb, rubidium; Sr, strontium; Y, yittrium; Zr, zirconium; Nb, Niobium; Ba, barium; La, lanthanum; Ce, cerium; m, meter; ‰, per mil; ND, not determined]

Sample identification No. Borehole Borehole depth (m) Strati-graphic unit Rb Sr Y Zr Nb Ba La Ce Analysis type 87Sr/86Sr (±0.00005 2σ) δ87Sr, ‰ (±0.07 2σ) δ87Srt, ‰ Seawater 87Sr/86Srpsw used
UE25a3–142 UE–25 a #3 43.3 Mc/MDg 48 89 45 320 16 115 ND ND WR 0.71554 8.94 10.4 0.7082
UE25a3–324 UE–25 a #3 98.8 Mc/MDg 90 176 41 173 20 182 ND ND WR .71616 9.81 11.4 .7081
UE25a3–493 UE–25 a #3 150.4 Mc/MDg 54 91 42 282 20 ND ND WR .71795 12.34 14.0 .7080
UE25a3–684 UE–25 a #3 208.4 Mc/MDg 84 177 44 212 21 210 ND ND WR .71539 8.73 10.5 .7079
UE25a3–863 UE–25 a #3 263.1 Mc/MDg 77 159 49 273 19 189 ND ND WR .71523 8.50 10.5 .7078
UE25a3–1069 UE–25 a #3 325.7 Mc/MDg 80 205 43 189 20 240 ND ND WR .71494 8.09 10.2 .7077
UE25a3–1430 UE–25 a #3 435.9 Mc/MDg 78 74 27 117 9 1,247 ND ND WR .71633 10.05 12.2 .7077
UE25a3–1722 UE–25 a #3 525.0 Mc/MDg 146 65 32 151 14 1,575 ND ND WR .72022 15.54 17.4 .7079
UE25a3–1846 UE–25 a #3 562.5 Mc/MDg 61 86 26 137 15 889 ND ND WR .72087 16.46 18.3 .7080
UE25a3–2093 UE–25 a #3 637.9 Mc/MDg 39 51 15 96 6 394 ND ND WR .72369 20.43 22.1 .7081
UE25a3–2287 UE–25 a #3 697.2 Mc/MDg 71 131 31 176 7 299 ND ND WR .71700 11.00 12.5 .7082
UE25a3–2432 UE–25 a #3 741.1 Du 2 87 33 6 2 ND ND WR .71323 5.68 7.10 .7082
UE25a3–2492 UE–25 a #3 759.6 Du 0 60 5 3 0 73 21 3 HCl-L .71111 2.69 4.04 .7083
UE25a3–2514 UE–25 a #3 766.4 Du 0 36 5 2 0 38 24 6 HCl-L .71080 2.26 3.60 .7083
HD–622 UE–25 p #1 1,277.7 DSlm 0 68 0 14 0 10 5 11 HCl-L .70907 - .19 .38 .7088
HD–621 UE–25 p #1 1,284.1 DSlm 0 62 0 11 0 0 9 0 HCl-L .70905 - .21 .35 .7088
UE25p 1–5900 UE–25 p #1 1,798.3 Sr 3 70 5 15 0 0 23 14 HCl-L .70835 -1.20 - .07 .7084

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