Geothermal resource assessment in Oklahoma

Conference · Thu Jul 01 00:00:00 EDT 1982

OSTI ID:7369499

Harrison, W E ^[1]; Luza, K V; Prater, M L; Cheung, P K; Ruscetta, C A ^[2]

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1. Oklahoma Geological Survey, Norman
2. ed.

The procedures and methods used to develop a geothermal gradient map of Oklahoma are discussed. Two areas, Haskell and Pittsburg Counties, in the Arkoma Basin, are discussed in detail. Three sandstone units, the Spiro, Cromwell, and Hartshorne were selected as potential low-temperature geothermal water sources. The average temperature ranged from 103/sup 0/F at Hartshorne to 158/sup 0/F at Cromwell. (MJF)

• OSTI ID: 7369499
• Report Number(s): DOE/ID/12079-71-Vol.1; ESL-98-Vol.1; CONF-820491-Vol.1-12; ON: DE82019912
• Resource Relation: Conference: Geothermal energy exploration and resource assessment technical conference, Salt Lake City, UT, USA, 5 Apr 1982; Related Information: In: Geothermal direct heat program roundup technical conference proceedings, by
• Country of Publication: United States
• Language: English

Related Subjects

15 GEOTHERMAL ENERGY
GEOTHERMAL RESOURCES
RESOURCE ASSESSMENT
OKLAHOMA
GEOTHERMAL GRADIENTS
MAPS
SANDSTONES
TEMPERATURE LOGGING
WELL TEMPERATURE
FEDERAL REGION VI
NORTH AMERICA
RESERVOIR TEMPERATURE
RESOURCES
ROCKS
SEDIMENTARY ROCKS
TEMPERATURE GRADIENTS
USA
WELL LOGGING
Geothermal Legacy
150301* - Geothermal Exploration & Exploration Technology- Geophysical Techniques & Surveys