Numerical simulation of magmatic hydrothermal systems
The dynamic behavior of magmatic hydrothermal systems entails coupled and nonlinear
multiphase flow, heat and solute transport, and deformation in highly heterogeneous media …
multiphase flow, heat and solute transport, and deformation in highly heterogeneous media …
Progress in deciphering the controls on the geochemistry of fluids in seafloor hydrothermal systems
SE Humphris, F Klein - Annual review of marine science, 2018 - annualreviews.org
Over the last four decades, more than 500 sites of seafloor hydrothermal venting have been
identified in a range of tectonic environments. These vents represent the seafloor …
identified in a range of tectonic environments. These vents represent the seafloor …
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
T Driesner, CA Heinrich - Geochimica et Cosmochimica Acta, 2007 - Elsevier
Realistic simulations of fluid flow in geologic systems have severely been hampered by the
lack of a consistent formulation for fluid properties for binary salt–water fluids over the …
lack of a consistent formulation for fluid properties for binary salt–water fluids over the …
Chemistry of hydrothermal vent fluids from the Main Endeavour Field, northern Juan de Fuca Ridge: Geochemical controls in the aftermath of June 1999 seismic …
In June 1999, an intense swarm of earthquakes occurred on the Endeavour segment of the
Juan de Fuca Ridge influencing hydrothermal activity in and around the Main Endeavour …
Juan de Fuca Ridge influencing hydrothermal activity in and around the Main Endeavour …
The structure and dynamics of mid-ocean ridge hydrothermal systems
Sub-seafloor hydrothermal convection at mid-ocean ridges transfers 25% of the Earth's heat
flux and can form massive sulfide ore deposits. Their three-dimensional (3D) structure and …
flux and can form massive sulfide ore deposits. Their three-dimensional (3D) structure and …
A thermodynamic explanation for black smoker temperatures
There is a remarkable difference between the maximum temperature of black smoker
effluent (350° C–400° C) and the temperature of the solidifying magma which heats it (∼ …
effluent (350° C–400° C) and the temperature of the solidifying magma which heats it (∼ …
[PDF][PDF] Submarine lava flow emplacement at the East Pacific Rise 9 50′ N: Implications for uppermost ocean crust stratigraphy and hydrothermal fluid circulation
The injection of magma, eruption of lava and tectonic stresses associated with seafloor
spreading at the global MOR crest profoundly impact the structure and permeability of the …
spreading at the global MOR crest profoundly impact the structure and permeability of the …
High‐temperature seawater circulation throughout crust of oceanic ridges: A model derived from the Oman ophiolites
A Nicolas, D Mainprice… - Journal of Geophysical …, 2003 - Wiley Online Library
We describe here the high‐temperature (HT∼ 700° C) and very high temperature (VHT∼
1000° C) recharge and discharge systems which are responsible for HT‐VHT hydrothermal …
1000° C) recharge and discharge systems which are responsible for HT‐VHT hydrothermal …
Temporal variability and tidal modulation of hydrothermal exit‐fluid temperatures at the Lucky Strike deep‐sea vent field, Mid‐Atlantic Ridge
We deployed autonomous temperature sensors at black smoker chimneys, cracks, and
diffuse flow areas at the Lucky Strike hydrothermal field (Mid‐Atlantic Ridge,~ 37° 17'N) …
diffuse flow areas at the Lucky Strike hydrothermal field (Mid‐Atlantic Ridge,~ 37° 17'N) …
Numerical investigation of transient hydrothermal processes around intrusions: Heat-transfer and fluid-circulation controlled mineralization patterns
New insights on the circulation of fluids around magmatic intrusions have been obtained
through coupled hydrothermal numerical modelling that takes into account i) a continuous …
through coupled hydrothermal numerical modelling that takes into account i) a continuous …