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Stable isotope data for sulfur, oxygen, and hydrogen in minerals and gases and electron microprobe data for minerals from Sulphur Bank mercury mine, Lake County, California

Dates

Publication Date
Start Date
2023-01-03
End Date
2023-10-24

Citation

Johnson, C.A., Muller, D.E., Alpers, C.N., Peek, S.E., Lowers, H.A., and Arribas, A., 2024, Stable isotope data for sulfur, oxygen, and hydrogen in minerals and gases and electron microprobe data for minerals from Sulphur Bank mercury mine, Lake County, California: U.S. Geological Survey data release, https://doi.org/10.5066/P9EQFOXX.

Summary

Stable isotope compositions (the ratios deuterium/hydrogen, oxygen-18/oxygen-16, and sulfur-34/sulfur-32) are reported for alunite, jarosite, kaolinite, silica, cinnabar, marcasite, and native sulfur from outcrops in and around the workings of the Sulphur Bank mercury mine, Lake County, California, and chemical compositions are reported, from electron microprobe analyses, for alunite and buddingtonite. Isotope analyses are given also for hydrogen sulfide gas from active fumaroles and for soluble sulfate in samples of mine waste. The waste results reflect fine grained material (particles less than 0.063 millimeter in diameter) that were taken from composites, each composite representing a particular waste pile that was active during [...]

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Attached Files

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1_SampleList.csv 4.08 KB text/csv
2_Hisotopes.csv 1.89 KB text/csv
3_Sisotopes.csv 3.64 KB text/csv
4_AluniteOisotopes.csv 871 Bytes text/csv
5_SilicateOisotopes.csv 395 Bytes text/csv
6_SolubleSulfateOisotopes.csv 669 Bytes text/csv
7_EMPalunite.csv 13.72 KB text/csv
8_EMPbuddingtonite.csv 1.87 KB text/csv
SulphurBankMercury_TIF_Files.zip 275.51 MB application/zip

Purpose

The data were collected to help achieve three objectives. The first objective was to develop a modern genetic model for ores that were an important source of mercury and sulfur for the United States in the late 19th century and early 20th century. The Sulphur Bank locality provides an exceptional natural laboratory for research in ore genesis because the ore forming system is still active; mercury- and sulfur-bearing minerals continue to precipitate today from upwelling hydrothermal fluids. The second objective is to improve the understanding of stable isotope systematics of geothermal environments situated above the water table, which are traditionally referred to as steam-heated environments. The third objective is to establish isotopic signatures of the various sulfur reservoirs at the Sulphur Bank site so that stable isotope analysis can be used to identify source(s) of sulfuric acid in groundwater and surface waters. Sources of acidity are of interest because the acid content of the waters may influence the degree to which the waters can leach and remobilize mercury and other metals from rocks and legacy mine waste.

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  • USGS Data Release Products
  • USGS Geology, Geophysics, and Geochemistry Science Center

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DOI https://www.sciencebase.gov/vocab/category/item/identifier doi:10.5066/P9EQFOXX

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