Application of fluid dynamics principles in tilted permeable media to terrestrial hydrothermal systems
- 1 February 1991
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 18 (2) , 199-202
- https://doi.org/10.1029/91gl00216
Abstract
No abstract availableThis publication has 17 references indexed in Scilit:
- Oxygen isotope map of the giant metamorphic-hydrothermal system around the northern part of the Idaho batholith, U.S.A.Applied Geochemistry, 1990
- Chapter 3. ISOTOPIC EXCHANGE in OPEN and CLOSED SYSTEMSPublished by Walter de Gruyter GmbH ,1986
- Strontium and oxygen isotopic variations in Mesozoic and Tertiary plutons of central IdahoContributions to Mineralogy and Petrology, 1985
- Pressure--Temperature--Time Paths of Regional Metamorphism I. Heat Transfer during the Evolution of Regions of Thickened Continental CrustJournal of Petrology, 1984
- Permeability of crystalline rocks: New in situ measurementsJournal of Geophysical Research, 1984
- The role of the fluid phase during regional metamorphism and deformationJournal of Metamorphic Geology, 1983
- A case study of the amount and distribution of heat and fluid during metamorphismContributions to Mineralogy and Petrology, 1980
- Natural convection in a sloping porous layerJournal of Fluid Mechanics, 1973
- Stability of the flow in a differentially heated inclined boxJournal of Fluid Mechanics, 1971
- Turbulent free convection in a vertical slotJournal of Fluid Mechanics, 1965