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VILLAS, R. N.; NORTON, D. Irreversible mass transfer between circulating hydrothermal fluids and the mayflower stock. Geologic, v. 72, p. 1471-1504, 1977.

RESUMO

Heat and mass transport processes related to the Mayflower stock in the Park City district, Utah, have been simulated using calculations based on geological observations and numerical methods which approximate convective and conductive heat transfer in permeable media. Permeability and flow porosity values for the Mayflower stock were estimated on the basis of a planar fracture model and data on the abundances and apertures of continuous fractures. Estimated permeabilities ranged from 4 x 10 -9 to 10 -7 cm2 and were hypothesized to represent initial permeabilities at the onset of the hydrothermal fluid circulation.

 
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