Structural Geology and Petroleum Potential of the South Flank of the Uinta Mountain Uplift, Northeastern Utah

Utah Geology Pub Date : 1900-01-01 DOI:10.34191/ug-2-2_129
J. Campbell
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引用次数: 1

Abstract

The transition between the Uinta basin and the Uinta uplift is masked by Tertiary and Quaternary sediments, so that both the position and the structural style of the boundary are unclear. Seismic data and recently drilled wells help to clarify the character of the boundary as having upthrust geometry, which is typical of the Rocky Mountain foreland. The structural configuration thus interpreted is significant to petroleum entrapment in a zone paralleling the entire south flank of the Uinta Mountains.
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犹他州东北部尤塔山隆起南侧构造地质与油气潜力
温塔盆地与温塔隆起之间的过渡被第三纪和第四纪的沉积所掩盖,使得边界的位置和构造样式都不明确。地震资料和最近钻探的井有助于澄清该边界具有上冲构造的特征,这是落基山脉前陆的典型特征。由此解释的构造形态对与整个乌塔山脉南侧平行的区域的油气圈闭具有重要意义。
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Currents of Great Salt Lake, Utah Sedimentary Cycles in the Nugget Sandstone, Northeastern Utah Largest Known Landslide of Its Type in the United States- A Failure by Lateral Spreading in Davis County, Utah Primary and Secondary Sedimentary Structures in Oil Shale and Other Fine-grained rocks, Green River Formation (Eocene), Utah and Colorado Bibliography of Utah Geology 1973
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