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    Fracture pattern study, Bull Canyon, Montrose and San Miguel counties, Colorado

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    http://hdl.handle.net/11166/83549
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    cogjm.Fracture_Pattern_Study_Bull_Cnyn_Montrose_San_Miguel_Ctys_CO_Sept_1957.pdf (1.435Mb)
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    Abstract
    A study was made of the joint patterns in four different formations exposed in Bull Canyon, and of favorable and unfavorable ground in the upper ore-bearing sandstone unit of the Salt Wash member of the Jurassic Morrison formation, from which about two-thirds of the uranium production in Bull Canyon has come. Two major joint sites sets were found in all formations, forming a conjugate system, striking N 50-60° W and N 30-40° E. Most prominent are the northwestward joints, which are approximately parallel to the adjacent Paradox Valley and Gypsum Valley anticlines.
    Author(s)
    Dalrymple, J. W., Jr.; Young, N. B.; Ulibarri, A.

    Date
    1957-09
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    • DOE/AEC Uranium Reports

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