Vitrinite reflectance of sinkhole coals, east central Missouri fire clay district
- Univ. of Missouri, Rolla, MO (United States). Dept. of Geology and Geophysics
East central Missouri contains numerous sinkholes many of which are filled with commercial quantities of fire clay and some contain small amounts of coal. Vitrinite reflectance averages from 513 samples taken from eleven of these coals ranged from 0.71 to 0.78. Data were remarkably consistent and no local trends were observed. Using Barker and Goldstein (1990) and Barker and Pawlewicz (1986) temperature correlations, these measurements suggest that the coals have been heated to temperatures on the order of 108 C to 128 C (average = 116). These temperatures are considered anomalously high when compared against known geothermal gradients and burial depths for these rocks. The temperatures suggest that the sinkhole coals have been heated by some thermal event, possibly associated with Mississippi Valley type mineralization. These temperatures are consistent with regional trends in the state. This data, when combined with other vitrinite reflectance and fluid inclusion data (right), suggest that southwest Missouri (Tristate) and southeast Missouri (Viburnum Trend) were hot spots, and that temperatures decrease regionally away from these two areas.
- OSTI ID:
- 5071025
- Report Number(s):
- CONF-9303210-; CODEN: GAAPBC
- Journal Information:
- Geological Society of America, Abstracts with Programs; (United States), Vol. 25:3; Conference: 27. annual Geological Society of America (GSA) North-Central Section meeting, Rolla, MO (United States), 29-30 Mar 1993; ISSN 0016-7592
- Country of Publication:
- United States
- Language:
- English
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Related Subjects
58 GEOSCIENCES
COAL DEPOSITS
GEOLOGY
GEOTHERMOMETRY
MISSOURI
VITRINITE
OPTICAL PROPERTIES
GEOLOGIC HISTORY
DEVELOPED COUNTRIES
GEOLOGIC DEPOSITS
MACERALS
MINERAL RESOURCES
NORTH AMERICA
PHYSICAL PROPERTIES
RESOURCES
USA
011000* - Coal
Lignite
& Peat- Reserves
Geology
& Exploration
580000 - Geosciences