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dc.contributor.authorHeiner, L.E.
dc.contributor.authorBeistline, E.H.
dc.contributor.authorMoody, D.W.
dc.contributor.authorThomas, B.I.
dc.contributor.authorWallis, J.E.
dc.contributor.authorLoperfido, J.C.
dc.contributor.authorPeterson, R.J.
dc.contributor.authorWolff, E.N.
dc.date.accessioned2012-11-05T19:38:11Z
dc.date.available2012-11-05T19:38:11Z
dc.date.issued1967
dc.identifier.citationHeiner, L.E., Beistline, E.H., Moody, D.W., Thomas, B.I., Wallis, J.E., Loperfido, J.C., Peterson, R.J., and Wolff, E.N., 1967, Geochemical-geophysical investigations, Fairbanks district: University of Alaska Mineral Industry Research Laboratory Report No. 12, 133 p., 11 sheets.en_US
dc.identifier.urihttp://hdl.handle.net/11122/1061
dc.description.abstractTrace element distribution in a subarctic valley in the Cleary Hill area of the Fairbanks gold district has been studied. Zinc and arsenic have been found excellent pathfinder elements for auriferous deposits. Methods of analysis for copper, lead, zinc, molybdenum, silver and arsenic as well as heavy metals are discussed. The University of Alaska method #2 has been improved, Terrain, slope, and frozen ground have little effect upon the distribution of trace elements associated with the Cleary H i l l vein. A new method for the determination of zinc using dilute acid is proposed. Analysis of geochemical data by trend surface procedures proved effective for localization of anomalies.en_US
dc.publisherUniversity of Alaska Mineral Industry Research Laboratoryen_US
dc.relation.ispartofseriesMIRL Report;no.12
dc.subjectCleary Hillen_US
dc.subjectFairbanksen_US
dc.subjectauriferous depositsen_US
dc.subjectgeochemicalen_US
dc.subjectgeophysicalen_US
dc.titleGeochemical-geophysical investigations, Fairbanks districten_US
dc.typeTechnical Reporten_US
refterms.dateFOA2020-01-24T15:28:20Z


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