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Thomas Driesner

Researcher at ETH Zurich

Publications -  105
Citations -  4095

Thomas Driesner is an academic researcher from ETH Zurich. The author has contributed to research in topics: Geothermal gradient & Hydrothermal circulation. The author has an hindex of 32, co-authored 91 publications receiving 3301 citations.

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The system H2O–NaCl. Part I: Correlation formulae for phase relations in temperature–pressure–composition space from 0 to 1000 °C, 0 to 5000 bar, and 0 to 1 XNaCl

TL;DR: In this article, a set of correlations describing the phase stability relations in the system H 2 O-NaCl is developed, including the vapor pressure of halite and molten NaCl, the NaCl melting curve, the composition of a halite-saturated liquid and vapor, the pressure of vapor+ liquid+halite coexistence, the temperature-pressure and temperature-composition relations for the critical curve, and the compositions of liquid and vapour on the vapor+liquid coexistence surface.
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The system H2O–NaCl. Part II: Correlations for molar volume, enthalpy, and isobaric heat capacity from 0 to 1000 °C, 1 to 5000 bar, and 0 to 1 XNaCl

TL;DR: In this paper, a set of correlations for the volumetric properties and enthalpies of phases in the system H2O-NaCl as a function of temperature, pressure, and composition has been developed that yields accurate values from 0 to 1000°C, 1 to 5000 bar, and 0 to 1 XNaCl.
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Porphyry-Copper Ore Shells Form at Stable Pressure-Temperature Fronts Within Dynamic Fluid Plumes

TL;DR: Numerical modeling shows that dynamic permeability responses to magmatic fluid expulsion can stabilize a front of metal precipitation at the boundary between lithostatically pressured up-flow of hot magmatic fluids and hydrostatically pressured convection of cooler meteoric fluids.
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Numerical simulation of magmatic hydrothermal systems

TL;DR: In this paper, the authors present a numerical solution of coupled partial differential equations and complementary equations of state (EOS) for the complete H2O-NaCl-CO2 system.
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The seismo-hydromechanical behavior during deep geothermal reservoir stimulations: open questions tackled in a decameter-scale in situ stimulation experiment

TL;DR: The In situ Stimulation and Circulation (ISC) experiment at the Grimsel Test Site in Switzerland as discussed by the authors was designed to address open research questions in a naturally fractured and faulted crystalline rock mass, and two hydraulic injection phases were executed to enhance the permeability of the rock mass.