--> ABSTRACT: Surface Thermal Maturity Map of Uinta, Piceance, and Eagle Basins Area, Utah and Colorado, by Vito F. Nuccio and Ronald C. Johnson; #91030 (2010)

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Surface Thermal Maturity Map of Uinta, Piceance, and Eagle Basins Area, Utah and Colorado

Vito F. Nuccio, Ronald C. Johnson

Knowledge of thermal maturity is essential for basin analysis studies because heat and heat flow play major roles in mineral formation, hydrocarbon generation and destruction, ground-water flow, and petroleum reservoir quality.

We studied the thermal maturity of several hundred outcrop samples of coal and carbonaceous shale from Pennsylvanian through Quaternary rocks in the area encompassing the Uinta, Piceance, and Eagle basins of Utah and Colorado. All samples were analyzed for mean random vitrinite reflectance (Rm); thus, thermal maturity is defined by Rm for this study.

Our data show that Rm generally increases with age of the rock, reflecting increasing burial depth and residence time at maximum temperature. Some coals show local anomalously high maturities because of proximity to Tertiary intrusives. Rocks of the same age show a general decrease in maturity from south to north in all three basins, which probably results from a decrease in geothermal gradients from south to north. In the Uinta basin, Rm values range from about 0.40 to 0.70% around the margins of the basin to 0.45% in the Altamont-Bluebell oil field near the basin center. In the Piceance basin, Rm values range from about 0.50 to 0.70% around the margins to about 0.25 to 0.35% in the center. The Eagle basin shows the widest range of Rm value , from 0.30 to 0.50% around the margins to values in the 4.0% range near the center.

Some vitrinite anomalies in the study area are best explained by sampling and analytical problems, such as choosing recycled vitrinite grains from organically lean shales or collecting weathered, oxidized samples.

AAPG Search and Discovery Article #91030©1988 AAPG Annual Convention, Houston, Texas, 20-23 March 1988.