Geochemistry of surface waters associated with an undisturbed Zn–Pb massive sulfide deposit: Water–rock reactions, solute sources and the role of trace carbonate
- 3 December 2010
- journal article
- Published by Elsevier BV in Chemical Geology
- Vol. 279 (1-2), 40-54
- https://doi.org/10.1016/j.chemgeo.2010.10.002
Abstract
No abstract availableKeywords
Funding Information
- Geological Survey of Canada
This publication has 37 references indexed in Scilit:
- Sustained sulfide oxidation by physical erosion processes in the Mackenzie River basin: Climatic perspectivesGeology, 2007
- Relative contributions of silicate and carbonate rocks to riverine Sr fluxes in the headwaters of the GangesGeochimica et Cosmochimica Acta, 2005
- Chemical denudation rates of the western Canadian orogenic belt: the Stikine terraneChemical Geology, 2003
- Mineralogic controls on the composition of natural waters dominated by silicate hydrolysisAmerican Journal of Science, 2002
- REE fractionation during granite weathering and removal by waters and suspended loads: Sr and Nd isotopic evidenceGeochimica et Cosmochimica Acta, 2001
- Global silicate weathering and CO2 consumption rates deduced from the chemistry of large riversChemical Geology, 1999
- Chemical and physical denudation in the Amazon River BasinChemical Geology, 1997
- The influence of parent material on small-scale spatial changes in streamwater chemistry in Scottish upland catchmentsJournal of Hydrology, 1997
- Chemical weathering in glacial environmentsGeology, 1997
- Variation in stream water chemistry and hydrograph separation in a small drainage basinJournal of Hydrology, 1996