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Title: Surface thermal maturity map of Uinta, Piceance, and Eagle basins area, Utah and Colorado

Conference ·
OSTI ID:6135678

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. The authors 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 (R/sub m/); thus, thermal maturity is defined by R/sub m/ for this study. The authors' data show that R/sub m/ generally increase with age of the rock, reflecting increase 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, R/sub m/ 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, R/sub m/ 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 R/sub m/ values, from 0.30 to 0.50% around the margins to values in the 4.0% range near the center.

OSTI ID:
6135678
Report Number(s):
CONF-880301-
Resource Relation:
Conference: Annual meeting of the American Association of Petroleum Geologists, Houston, TX, USA, 20-23 Mar 1988
Country of Publication:
United States
Language:
English