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Occurrence and distribution of barite in the permo-triassic siksikpuk formation along the Brooks Range haul road

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dc.contributor.author Payne, M.W.
dc.date.accessioned 2013-08-27T18:57:43Z
dc.date.available 2013-08-27T18:57:43Z
dc.date.issued 1980-03
dc.identifier.citation Payne, 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.uri http://hdl.handle.net/11122/2156
dc.description.abstract Barite 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.tableofcontents Introduction -- Geologic setting -- Atigun Gorge section -- Barite -- Occurrence -- Origin -- Quantity -- Conclusion -- References. en_US
dc.language.iso en_US en_US
dc.publisher University of Alaska Mineral Industry Research Laboratory en_US
dc.title Occurrence and distribution of barite in the permo-triassic siksikpuk formation along the Brooks Range haul road en_US
dc.type Technical Report en_US


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