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Title Kinetics of the smectite to illite transformation in the Denver Basin: Clay mineral, K-Ar data, and mathematical model results
Creator/Author Elliot, W.C. ; Aronson, J.L. ; Matisoff, G. (Case Western Reserve Univ., Cleveland, OH (United States)) ; Gautier, D.L. (Geological Survey, Denver, CO (United States))
Publication Date1991 Mar 01
OSTI IdentifierOSTI ID: 5750242
Other Number(s)ISSN0149-1423; CODEN: AABUD
Resource TypeJournal Article
Resource RelationAAPG Bulletin (American Association of Petroleum Geologists) ; Vol/Issue: 75:3
Subject580000 -- Geosciences ;030200 -- Natural Gas-- Reserves, Geology, & Exploration; COLORADO-- NATURAL GAS DEPOSITS;ILLITE-- ISOTOPE DATING;ILLITE-- MATURATION;ILLITE-- REACTION KINETICS;SMECTITE-- HYDROTHERMAL ALTERATION;SMECTITE-- ISOTOPE DATING;SMECTITE-- MATURATION;SMECTITE-- REACTION KINETICS; ARGON ISOTOPES;BENTONITE;CRETACEOUS PERIOD;GEOCHEMISTRY;GEOLOGIC HISTORY;MATHEMATICAL MODELS;POTASSIUM ISOTOPES;SEDIMENTARY BASINS
Related SubjectAGE ESTIMATION;ALKALI METAL ISOTOPES;CHEMISTRY;CLAYS;DEVELOPED COUNTRIES;FEDERAL REGION VIII;GEOLOGIC AGES;GEOLOGIC DEPOSITS;GEOLOGIC STRUCTURES;INORGANIC ION EXCHANGERS;ION EXCHANGE MATERIALS;ISOTOPES;KINETICS;MATERIALS;MESOZOIC ERA;MINERAL RESOURCES;MINERALS;NORTH AMERICA;RESOURCES;SILICATE MINERALS;USA
Description/Abstract Clay mineral data, potassium-argon (K-Ar) ages, and mathematical model simulations indicate the important kinetic factors controlling the smectite to illite transformation (illitization) in Upper Cretaceous Mowry and Niobrara core and outcrop bentonites from the Denver basin.^The data also provide additional information on the thermal history of the basin.^Data show that both the percentages of illite layers and the K-Ar ages of mixed layer illite-smectite (I/S) increase with increasing depths of burial, and this trend was simulated mathematically employing a very simplified burial model with a fifth-order overall kinetic expression for the information of illite.^For most of the basin, the data is compatible with I/S having been formed in response to increased temperature from progressive burial, because the oldest K-Ar ages of I/S are from the deepest buried I/S along the basin axis.^In addition, these data qualitatively suggest that I/S even as small as <0.1 {mu}m retains radiogenic argon under Denver basin burial temperatures.^I/S separated from drill core bentonites from the Watenberg gas field, astride the basin axis and known to have been subjected to an anomalously high temperature history, are the most illitic and among the oldest measured from core in this study.^The ages of illitization (about 60 Ma) are coincident with the Laramide time of structural development of the basin and uplift of the Front Range.^The reconstructions of the burial history, and the modeling of the timing and extent of illitization, suggest that the area of the Wattenberg as field was an upper Cretaceous depocenter, an area of relatively deeper burial along the basin axis.
Country of PublicationUnited States
LanguageEnglish
FormatPages: 436-462
System Entry Date2001 May 13

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