This is a PDF-only article. The first page of the PDF of this article appears above.
This article requires a subscription to view the full text. If you have a subscription you may use the login form below to view the article. Access to this article can also be purchased.
Log in using your username and password
Purchase access
You may purchase access to this article. This will require you to create an account if you don't already have one.
In this issue
Jump to section
Related Articles
Cited By...
- Temperature-dependent estimation of Gibbs energies using an updated group contribution method
- Thermodynamic modelling of fluids from surficial to mantle conditions
- Reactive transport modelling of compacting siliciclastic sediment diagenesis
- An internally consistent thermodynamic dataset for aqueous species in the system Ca-Mg-Na-K-Al-Si-O-H-C-Cl to 800 {degrees}C and 5 kbar
- Partitioning of Chlorine Between Nacl Brines and Ferro-Pargasite: Implications For the Formation of Chlorine-Rich Amphiboles In Mafic Rocks
- Sulfur Oxidation Genes in Diverse Deep-Sea Viruses
- The Chemistry of Carbon in Aqueous Fluids at Crustal and Upper-Mantle Conditions: Experimental and Theoretical Constraints
- Thermodynamic Modeling of Fluid-Rock Interaction at Mid-Crustal to Upper-Mantle Conditions
- GEM-SELEKTOR GEOCHEMICAL MODELING PACKAGE: TSolMod LIBRARY AND DATA INTERFACE FOR MULTICOMPONENT PHASE MODELS
- Constraining Compositions of Hydrothermal Fluids in Equilibrium with Polymetallic Ore-Forming Sulfide Assemblages
- Acid production by FeSO4{middle dot}nH2O dissolution and implications for terrestrial and martian aquatic systems
- Thermodynamic Databases for Water-Rock Interaction
- Two-dimensional reactive transport modeling of CO2 injection in a saline aquifer at the Sleipner site, North Sea
- Deriving formation constants for aqueous metal complexes from XANES spectra: Zn2+ and Fe2+ chloride complexes in hypersaline solutions
- Hydrothermal Transport and Deposition of Rhenium under Subcritical Conditions(up to 200{degrees}C) in Light of Experimental Studies
- Modeling Multiphase Non-isothermal Fluid Flow and Reactive Geochemical Transport in Variably Saturated Fractured Rocks: 1. Methodology
- Solubility and stability of zeolites in aqueous solution: II. Calcic clinoptilolite and mordenite
- Hydrothermal pore fluid pressure and the stability of porous, permeable volcanoes