Subsurface Reinterpretation of Ordovician and Devonian Strata in Southwest Wyoming with Implications for Upwarping Across the Transcontinental Arch
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Published:2018-07
Issue:3
Volume:55
Page:91-118
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ISSN:0027-254X
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Container-title:The Mountain Geologist
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language:en
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Short-container-title:MT GEOL
Author:
Anderson Donna1, Longman Mark2
Affiliation:
1. Colorado School of Mines, Golden, CO 2. QEP Resources, Denver, CO
Abstract
A new interpretation of the subsurface geometries of the Ordovician Bighorn Dolomite and overlying Devonian strata across southwestern Wyoming arises from revising the stratigraphy in a core from the Mountain Fuel Supply UPRR #11–19–104–4 well drilled on the crest of the Rock Springs Uplift in 1962. One of only a few wells to penetrate all or part of the Lower Paleozoic succession in the subsurface of southwestern Wyoming, the well was almost continuously cored through the Devonian–Cambrian succession. From a reinterpretation of the stratigraphy in the core, 22 ft of Bighorn Dolomite is recognized based on the characteristic Thalassinoides bioturbation fabric in skeletal dolowackestone typical of Late Ordovician subtidal carbonate facies ranging from Nevada to Greenland along the western margin of the Great American Carbonate Bank. This lithology is in complete contrast with the alternating dolomitic flat-pebble conglomerate and dolomudstone of the underlying Cambrian Gallatin Limestone and the cyclical units of brecciated anhydritic dolomudstone and quartzose sandstone of the overlying Devonian Lower Member of the Jefferson Formation. Stratigraphic re-interpretation yields insights regarding Ordovician–Devonian stratal geometries across southwestern Wyoming. More widespread than previously portrayed, the Bighorn Dolomite pinches out on the eastern flank of the Rock Springs Uplift. Similar to past interpretations, Devonian strata pinch out east of the Rock Springs Uplift at Table Rock Field. A true-geometry multi-datumed stratigraphic cross section yields insights not obtainable by mapping. Regionally, top truncation of stratigraphic units below the base-Madison Limestone unconformity normally progresses stratigraphically deeper eastward. However, in southwestern Wyoming, the Devonian Lower Member of the Jefferson Formation overlaps the older Bighorn Dolomite by marked onlap across the Rock Springs Uplift and then pinches out by top truncation/onlap near Table Rock Field, forming an “abnormal” overlap relationship along the northern margin of the Transcontinental Arch. The underlying Bighorn Dolomite shows little to no onlap onto the underlying Cambrian section, but is markedly top truncated below the Lower Member of the Jefferson Formation. Comparing proportions of onlap versus top truncation for the two formations constrains the timing of two successive upwarping episodes along the northern margin of the Transcontinental Arch across southwestern Wyoming. The first is arguably Middle Devonian, and the second spans the Devonian–Mississippian boundary. Two subtle and different angular unconformities created by these two episodes imply a persistent fold or tilt axis that sequentially was reactivated along the northern margin of the Transcontinental Arch in southwestern Wyoming.
Publisher
Rocky Mountain Association of Geologists
Reference63 articles.
1. Amstrat, 1962, Log of Mountain Fuel Supply Union Pacific #4 11–19–104: Canstrat Corporation, Calgary, Alberta, Canada. 2. Asquith, G., and D. Krygowski, 2004, Basic well log analysis: American Association of Petroleum Geologists Methods in Exploration Series 16, 2nd edition, 244 p. 3. Baars, D.L., 1972, Devonian system, in W.W. Mallory, ed., Geologic atlas of the Rocky Mountain region: Rocky Mountain Association of Geologists, Denver, Colorado, p. 90–99. 4. Becker, R.T., R.M. Gradstein, and O. Hammer, 2012 The Devonian Period, in F.M. Gradstein, , J.G. Ogg, M. Schmitz, and G. Ogg, eds., The geologic time scale, 2012: Elsevier B.V., p. 559–601. 5. Bell, L.H., 1955, The geology of the southeastern flank of the Wind River Mountains, Fremont County, Wyoming: Ph.D. Dissertation, University of Wyoming, Laramie, Wyoming, 204 p.
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2 articles.
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