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Abstract
A steady-state solution for heat transfer from an isothermal, spherical magma chamber, with an imposed regional geothermal gradient far from the chamber, is developed. The extensive published heat-flow data set for Mount Hood, Oregon, is dominated by conductive heat transfer in the deeper parts of most drill holes and provides an ideal application of such a model. Magma-chamber volumes or depths needed to match the distribution of heat-flow data are larger or shallower than those inferred from geologic evidence.
| Publication type | Conference Paper |
|---|---|
| Publication Subtype | Conference Paper |
| Title | Conductive heat transfer from an isothermal magma chamber and its application to the measured heat flow distribution from mount hood, Oregon |
| ISBN | 0934412715 |
| Volume | 17 |
| Year Published | 1993 |
| Language | English |
| Publisher | Publ by Geothermal Resources Council |
| Publisher location | Davis, CA, United States |
| Larger Work Title | Transactions - Geothermal Resources Council |
| First page | 141 |
| Last page | 148 |
| Conference Title | Proceedings of the 1993 Annual Meeting on Utilities and Geothermal: An Emerging Partnership |
| Conference Location | Burlingame, CA, USA |
| Conference Date | 10 October 1993 through 13 October 1993 |
| Google Analytic Metrics | Metrics page |