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The AAPG/Datapages Combined Publications Database
Journal of Sedimentary Research (SEPM)
Abstract
Diagenesis of the Lower Permian Krider Member, Southwest Kansas, U.S.A.: Fluid-Inclusion, U-Pb, and Fission-Track Evidence for Reflux Dolomitization During Latest Permian Time
John A. Luczaj (1), Robert H. Goldstein (2)
ABSTRACT
Diagenesis of the lower Krider Member of the Nolans Limestone in the Hugoton embayment was dominated by dolomitization and subsequent anhydrite precipitation and replacement. Typical dolomite crystals have a replacive inclusion-rich core followed by a clear rim in transmitted light, and have three cathodoluminescent (CL) growth zones. Fission-track analysis suggests that most uranium resides in CL Zone 2, in an earlier dolomite zone replaced by Zone 2, and in enriched phosphatic minerals. Regionally, the most U-rich part of the lower Krider Member is an east-west oriented region in the north-central part of the Hugoton embayment. Uranium concentration does not correlate directly with lithology, location of tidal-flat deposits, or subaerial exposure surfaces. U and Pb concentrations for whole-rock dolostone analyses range from 12 to 29 ppm and from 1.4 to 6.7 ppm, respectively. Concordant U-Pb and Pb-Pb isochrons and a Total Pb/U concordia plot indicate that dolomitization took place around 250 Ma and that the timing of U enrichment was younger than the Early Permian depositional age.
Fluid-inclusion analyses suggest that the U-rich dolomitization took place at low temperatures in the presence of a Na-Ca-Mg-Cl brine and was followed by a later event that heated the rocks to at least 95°C. From fluid-inclusion data, petrographic and stratigraphic relationships, and U-Pb age dates from the dolomitic rocks, we suggest that during the Late Permian, reflux of low temperature (<50°C), Mg-bearing brines precipitated U-bearing dolomite and replaced earlier dolomite in the lower Krider Member and other units in the Chase Group. Some all-liquid fluid inclusions were later thermally reequilibrated by stretching after the Permian, possibly by either (1) later burial with a high geothermal gradient or by (2) hot, topography-driven fluid flow out of the Rocky Mountain foreland during the Tertiary.
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