| Title | Modelling of Kamphaeng Geothermal Reservoir |
|---|---|
| Authors | Hochstein, M.P., O'Sullivan, M.J. and Bhaddee, S. |
| Year | 1987 |
| Conference | New Zealand Geothermal Workshop |
| Keywords | |
| 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. |