The research of fluids in the earth's crust is greatly benefiting from methodological (analytical) and experimental advances and the rapid development of increasingly powerful numerical modelling systems. New experimental data continuously refine the accuracy of numerical models aiming to quantitatively reconstruct geological processes. Geological modelling programs have moved on from linear or 2-dimensional approaches to integrating 3 or 4D geology with geothermal aspects, fluids flow and reactive transport processes into complex, quantitative scenarios. These combinations of refinement of the data base and advances in computational capacities are the stepping stones for the development of the predictive quality of mineralising models and ...
International audienceIn fractured media, fluid flow depends on and induces coupled processes (hydro...
International audienceThe development of the Enhanced Geothermal System (EGS) at Soultz-sous-Forêts ...
Our research evaluates the hypothesis that feedback amongst thermal-chemical-mechanical processes op...
Traditionally, geologists focussed their research on the solid part of the subsurface. Increasingly ...
This special issue entitled “Geofluids and Energy for the XXI Century” focuses on cutting edge resea...
The 8th International Conference on Gas Geochemistry provided the opportunity for scientists from di...
This modern book stimulates the development of geochemistry in the earth sciences. The authors hav...
1. Introduction Fluid flow is a first-order feature of the geodynamic evolution of basins and orogen...
Section snippets Introduction of the special volume Fluids are ubiquitous in Earth's lithosphere. Re...
In this Special Issue, all aspects of fluid flow and heat transfer in geothermal applications, inclu...
Movement of water and other fluids in the Earth’s crust is critical to many geological processes, in...
The paper is an overview of the current status on experimental petrology — its objectives and its ma...
International audienceIn fractured media, fluid flow depends on and induces coupled processes (hydro...
This final report describes the results of a research program we carried out over a five-year (3/199...
Studying orogens-basins interaction requires a multi-scale approach that combines multi-methodologic...
International audienceIn fractured media, fluid flow depends on and induces coupled processes (hydro...
International audienceThe development of the Enhanced Geothermal System (EGS) at Soultz-sous-Forêts ...
Our research evaluates the hypothesis that feedback amongst thermal-chemical-mechanical processes op...
Traditionally, geologists focussed their research on the solid part of the subsurface. Increasingly ...
This special issue entitled “Geofluids and Energy for the XXI Century” focuses on cutting edge resea...
The 8th International Conference on Gas Geochemistry provided the opportunity for scientists from di...
This modern book stimulates the development of geochemistry in the earth sciences. The authors hav...
1. Introduction Fluid flow is a first-order feature of the geodynamic evolution of basins and orogen...
Section snippets Introduction of the special volume Fluids are ubiquitous in Earth's lithosphere. Re...
In this Special Issue, all aspects of fluid flow and heat transfer in geothermal applications, inclu...
Movement of water and other fluids in the Earth’s crust is critical to many geological processes, in...
The paper is an overview of the current status on experimental petrology — its objectives and its ma...
International audienceIn fractured media, fluid flow depends on and induces coupled processes (hydro...
This final report describes the results of a research program we carried out over a five-year (3/199...
Studying orogens-basins interaction requires a multi-scale approach that combines multi-methodologic...
International audienceIn fractured media, fluid flow depends on and induces coupled processes (hydro...
International audienceThe development of the Enhanced Geothermal System (EGS) at Soultz-sous-Forêts ...
Our research evaluates the hypothesis that feedback amongst thermal-chemical-mechanical processes op...