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dc.contributor.authorPayne, M.W.
dc.date.accessioned2013-08-27T18:57:43Z
dc.date.available2013-08-27T18:57:43Z
dc.date.issued1980-03
dc.identifier.citationPayne, M.W., 1980, Occurrence and distribution of barite in the permo-triassic siksikpuk formation along the Brooks Range haul road: University of Alaska Mineral Industry Research Laboratory Open File 80-7, 12 p.en_US
dc.identifier.urihttp://hdl.handle.net/11122/2156
dc.description.abstractBarite commonly occurs in Permian to Triassic age rocks along the north flank of the Brooks Range. The Siksikpuk Formation (Wolfcampian to lowest Guadalupian age) is noted for its barite and is well exposed in the vicinity of Galbraith Lake along the pipeline haul road (Figure 1). The proximity of these barite deposits to an existing road made them a logical selection for investigation. The study was designed to provide detailed stratigraphic information on barite quantity and quality, associated clay mineralogy, and relationship of barite to environments of deposition.en_US
dc.description.tableofcontentsIntroduction -- Geologic setting -- Atigun Gorge section -- Barite -- Occurrence -- Origin -- Quantity -- Conclusion -- References.en_US
dc.language.isoen_USen_US
dc.publisherUniversity of Alaska Mineral Industry Research Laboratoryen_US
dc.titleOccurrence and distribution of barite in the permo-triassic siksikpuk formation along the Brooks Range haul roaden_US
dc.typeTechnical Reporten_US
refterms.dateFOA2020-01-24T13:54:04Z


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