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Geochemical study of authigenic minerals in the Salt Wash Member of the Morrison Formation, Slick Rock District, San Miguel County, Colorado

Book ·
OSTI ID:6278322
Authigenic minerals were examined to evaluate the diagenetic history of this fluvial unit. The minerals were characterized petrographically, chemically, mineralogically and isotopically to define their geochemical environment of deposition. Minerals examined include albite, barite, calcite, chalcedony, chlorite, dolomite, illite-smectite, hematite, kaolinite, pyrite, quartz, and smectite. The minerals formed during three distinct episodes of diagenetic alteration: early diagenesis, late diagenesis and recent alterations. Early diagenetic minerals formed soon after deposition of the host rocks. The composition of the pore waters was largely a product of evaporation and interaction with felsic volcanic ash. These solutions were alkaline, and generally oxidizing; however, near detrital plant fragments, they were chemically reducing. During deep burial, two tectonically driven solutions entered the Morrison Formation through faults. These solutions precipitated calcite, barite, dolomite, and copper minerals and resulted in ferric oxide dissolution. The first of the solutions was a brine that originated in the evaporites of the Pennsylvanian Hermosa Formation. The second solution was a dilute, meteoric water. During Late Tertiary time into the Recent, units overlying the Morrison Formation were eroded. As the Morrison Formation was exposed, meteoric water flowed through structurally favored portions of the Salt Wash Member dissolving plagioclase and chlorite, and precipitating kaolinite.
Research Organization:
Colorado School of Mines, Golden (USA)
OSTI ID:
6278322
Country of Publication:
United States
Language:
English

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