1. High resolution schemes for hyperbolic conservation laws;Harten;J. Comput. Phys.,1983
2. The computer model HYDROTHERM, a three-dimensional finite-difference model to simulate ground-water flow and heat transport in the temperature range of 0 to 1, 200°C;Hayba
3. Multiphase groundwater flow near cooling plutons;Hayba;J. Geophys. Res.,1997
4. The response of ridge-crest hydrothermal systems to segmented, episodic magma supply;Haymon;Geol. Soc. Spec. Publ.,1996
5. Hydrothermal eruptions in the Waiotapu geothermal system, New Zealand: Their origin, associated breccias, and relation to precious metal mineralization;Hedenquist;Econ. Geol.,1985