Modelling of Kamphaeng Geothermal Reservoir
- Location
- San Kamphaeng, Thailand
- Conference
- New Zealand Geothermal Workshop
- Year
- 1987
- Session
- Modelling
- Language
- English
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Abstract
Temperature in deep exploration wells t h e prospect modelled by computing natural heat and mass transfer in a frncture zone. tectonic observed natural heat loss (35 isothrrm at drpth , fluid chemistry, and geophysical models provided important restraints for the model. The reservoir can be modelled as an inclined within fracture zone whose top has been sealed by mineral deposition; heat is most likely supplied by a decp convection cell standing in fractured granites (depths 5 km). The potential of reservoir is limited can bc predicted by the model.
Copyright 1987, University of Auckland. Readers who download papers from this site should honour the copyright of the original authors, and may not copy or distribute the work further without the permission of the original publisher.