Evolution of groundwater chemical composition by plagioclase hydrolysis in Norwegian anorthosites
- 1 March 2006
- journal article
- Published by Elsevier BV in Geochimica et Cosmochimica Acta
- Vol. 70 (6), 1337-1355
- https://doi.org/10.1016/j.gca.2005.11.025
Abstract
No abstract availableThis publication has 21 references indexed in Scilit:
- Mineralogic controls on the composition of natural waters dominated by silicate hydrolysisAmerican Journal of Science, 2002
- The chemistry of Norwegian groundwaters: IV. The pH-dependence of element concentrations in crystalline bedrock groundwatersScience of The Total Environment, 2001
- The chemistry of Norwegian groundwaters: III. The distribution of trace elements in 476 crystalline bedrock groundwaters, as analysed by ICP-MS techniquesScience of The Total Environment, 2000
- The chemistry of Norwegian groundwaters: I. The distribution of radon, major and minor elements in 1604 crystalline bedrock groundwatersScience of The Total Environment, 1998
- Hydrogeochemistry of Millstone Grit and Coal Measures groundwaters, south Yorkshire and north Derbyshire, UKQuarterly Journal of Engineering Geology, 1997
- The geochemistry, age, and origin of groundwater in a mafic pluton, East Bull Lake, Ontario, CanadaGeochimica et Cosmochimica Acta, 1990
- Some Observations on the Stoichiometry of Feldspar Hydrolysis in Granitic SoilJournal of Environmental Quality, 1988
- Chemical alteration in the micro weathering environment within a spheroidally-weathered anorthosite boulderGeochimica et Cosmochimica Acta, 1984
- A world model of soil carbon dioxideEarth Surface Processes and Landforms, 1983
- Origin of the Chemical Compositions of Some Springs and LakesPublished by American Chemical Society (ACS) ,1967