1992
DOI: 10.3133/ofr92419
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Analyses and descriptions of geochemical samples, southwestern part of the Dahlonega gold belt and vicinity, Georgia, and seven samples from Clay, Cleburne, and Tallapoosa counties, Alabama

Abstract: Semiquantitative spectrographic analyses for 30 elements, atomic absorption analyses for gold, copper, lead, and zinc, colorimetric analyses for arsenic and molybdenum, and instrumental analyses for mercury on all or part of a sample suite of 788 rock and saprolite samples are reported here in detail. Complete chemical analyses are reported on 27 fresh to partly weathered rock samples. Most of the samples are saprolite derived from mica schist and gneiss, amphibolite, and quartzite, or vein quartz in saprolite… Show more

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(4 citation statements)
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“…The distribution of the higher negative correlation coefficients also appears to be random. Similar results were found for samples from the northeastern half of the Dahlonega gold belt (Lesure, 1992).…”
Section: Discussion Of Sample Data and Conclusionsupporting
confidence: 84%
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“…The distribution of the higher negative correlation coefficients also appears to be random. Similar results were found for samples from the northeastern half of the Dahlonega gold belt (Lesure, 1992).…”
Section: Discussion Of Sample Data and Conclusionsupporting
confidence: 84%
“…In general, however, 13 percent of any rock type collected in outcrop and 78 percent of any rock type collected from a mine area contain detectable gold at a limit of detection of 0.02 ppm. Similar calculations for the northeastern half of the Dahlonega belt show that 24 percent of outcrop samples and 67 percent of mine samples are gold-bearing (Lesure, 1992).…”
Section: Bonner Minementioning
confidence: 65%
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