1 |
Fairley, J. P. (2009) Modeling fluid flow in a heterogeneous,fault-controlled hydrothermal system. Geofluids,v.9, p.153-166
DOI
ScienceOn
|
2 |
Harcouet-Menou, V., Guillou-Frottier, L., Bonneville, A.,Adler, P. M. and Mourzenko, V. (2009) Hydrothermalconvection in and around mineralized fault zones:Insights from two- and three-demensional numericalmodeling applied to the Ashanti belt, Ghana. Geofluids,v.9, p.116-137
DOI
ScienceOn
|
3 |
Simms, M. A. and Garven, G. (2004) Thermal convectionin faulted extensional sedimentary basins: theoreticalresults from finite-element modeling. Geofluids, v.4,p.109-130
DOI
ScienceOn
|
4 |
Smith, L. and Chapman, D. S. (1983) On the thermaleffects of groundwater flow, 1. Regional scale systems,Journal of Geophysical Research, v.88, p.593-608
DOI
|
5 |
Yang. J., Large, R. R. and Bull, S. W. (2004) Factors controllingfree thermal convection in faults in sedimentarybasins: implications for the formation of zincleadmineral deposits. Geofluids, v.4, p.237-247
DOI
ScienceOn
|
6 |
Lee, Y. and Deming, D. (1998) Evaluation of thermal conductivitytemperature corrections applied in terrestrialheat flow studies. Journal of Geophysical Research,v.103, p.2447-2454
DOI
ScienceOn
|
7 |
Bodvarsson, G. S., Benson, S. M. and Witherspoon, P. A.(1982) Theory of the development of geothermal systemscharged by vertical faults. Journal of GeophysicalResearch, v.87, p.9317-9328
DOI
|
8 |
Bodvarsson, G. S. and Tsang, C. F. (1982) Injection andthermal breakthrough in fractured geothermal reservoirs. Journal of Geophysical Research, v.87, p.1031-1048
DOI
|
9 |
Zhao, C., Hobbs, B. E., Ord, A., Kuhn, M., Muhlhaus, H.B. and Peng, S. (2006) Numerical simulation of double-diffusion driven convective flow and rock alterationin three-dimensional fluid-saturated geologicalfault zones. Computer Methods in Applied Mechanicsand Engineering, v.195, p.2816-2840
DOI
ScienceOn
|
10 |
Ehlers, T. A. and Chapman, D. S. (1999) Normal faultthermal regimes: conductive and hydrothermal heattransfer surrounding the Wasatch fault. Utah, Tectonophysics,v.312, p.217-234
DOI
ScienceOn
|
11 |
Deming, D. (2002) Introduction to hydrogeology. McGrawHill, New York, 468p
|
12 |
Samardzioska, T. and Popov, V. (2005) Numerical comparisonof the equivalent continuum, non-homogeneousand dual porosity models for flow and transportin fractured porous media. Advances in Water Resources, v.28, p.235-255
DOI
ScienceOn
|
13 |
Lopez, D. L. and Smith, L. (1996) Fluid flow in faultzones: Influence of hydraulic anisotropy and heterogeneityon the fluid flow and heat transfer regime.Water Resources Research, v.32, p.3227-3235
DOI
ScienceOn
|
14 |
Yang, J. (2006) Full e-D numerical simulation of hydrothermalfluid flow in faulted sedimentary basins:Example of the McArthur basin, northern Australia.Journal of Geochemical Exploration, v.89, p.440-444
DOI
ScienceOn
|
15 |
Bodvarsson, G. (1969) On the temperature of water flowingthrough fractures. Journal of Geophysical Research,v.74, p.1987-1992
DOI
|
16 |
Braun, J., Munroe, S. M. and Cox S. F. (2003) Transientfluid flow in and around fault. Geofluids, v. 3, p. 81-87
DOI
ScienceOn
|
17 |
Cook, P. G. (2003) A guide to regional groundwater flowin fractured rock aquifers. CSIRO, 108p
|
18 |
Zhao, C., Hobbs, B. E., Ord, A., Hornby, P., Muhlhaus, H.and Peng, S. (2008) Theoretical and numerical analysesof pore-fluid flow focused heat transfer aroundgeological faults and large cracks. Computers and Geotechnics,v.35, p.357-371
DOI
ScienceOn
|
19 |
Anderson, M. P. (2005) Heat as a ground water tracer. Ground Water, v.43, p.951-968
DOI
PUBMED
ScienceOn
|
20 |
Deming, D., Nunn, J. A. and Evans, D. G. (1990) Thermaleffects of compaction-driven groundwater flow fromoverthrust belts. Journal of Geophysical Research, v.95, p.6669-6683
DOI
|
21 |
Lopez, D. L. and Smith, L. (1995) Fluid flow in faultzones: Analysis of the interplay of convective circulationand topographically driven groundwater flow.Water Resources Research, v.31, p.1489-1503
DOI
ScienceOn
|