Water–rock interaction and acid neutralization in a large schist debris dam, Otago, New Zealand
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[1] D. Craw,et al. Gold mineralization without quartz veins in a ductile-brittle shear zone, Macraes Mine, Otago Schist, New Zealand , 1999 .
[2] R. W. Lawrence,et al. A method to calculate the neutralization potential of mining wastes , 1997 .
[3] S. Banwart,et al. The dissolution of biotite and chlorite at 25°C in the near-neutral pH region , 1996 .
[4] B. Kimball,et al. Effects of colloids on metal transport in a river receiving acid mine drainage, upper Arkansas River, Colorado, U.S.A. , 1995 .
[5] D. W. Smith,et al. Formation of authigenic Fe2+‐bearing smectite‐vermiculite during terrestrial diagenesis, southern New Zealand , 1995 .
[6] R. W. Lawrence,et al. On the neutralization of acid rock drainage by carbonate and silicate minerals , 1995 .
[7] L. Fernández-Díaz,et al. Fluid supersaturation and crystallization in porous media , 1995, Geological Magazine.
[8] B. Velde. Origin and mineralogy of clays , 1995 .
[9] B. Velde. Composition and Mineralogy of Clay Minerals , 1995 .
[10] D. Craw. Contrasting alteration mineralogy at an unconformity beneath auriferous terrestrial sediments, central Otago, New Zealand , 1994 .
[11] David W. Blowes,et al. Secondary minerals and acid mine-water chemistry , 1994 .
[12] C. Rochelle. Migration of Cement Pore Fluids from a Radioactive Waste Repository: Experimental Studies of Chlorite Dissolution Rates , 1994 .
[13] D. Craw,et al. Gold nugget growth during tectonically induced sedimentary recycling, Otago, New Zealand , 1993 .
[14] B. Roser,et al. Geochemical evidence for the position of the Caples–Torlesse boundary in the Otago Schist, New Zealand , 1992, Journal of the Geological Society.
[15] Patrick V. Brady,et al. The effect of silicate weathering on global temperature and atmospheric CO2 , 1991 .
[16] T. Pačes. The kinetics of base cation release due to chemical weathering , 1990 .
[17] D. Craw,et al. Origin and deposition of a graphitic schist-hosted metamorphogenic Au-W deposit, Macraes, East Otago, New Zealand , 1989 .
[18] J. Cherry,et al. Migration of acidic groundwater seepage from uranium-tailings impoundments, 1. Field study and conceptual hydrogeochemical model , 1988 .
[19] A. E. Greenberg,et al. Standard methods for the examination of water and wastewater : supplement to the sixteenth edition , 1988 .
[20] K. Hayes,et al. Geochemical processes at mineral surfaces , 1987 .
[21] D. Craw. Ferrous-iron-bearing vermiculite-smectite series formed during alteration of chlorite to kaolinite, Otago Schist, New Zealand , 1984, Clay Minerals.
[22] A. Lasaga. Chemical kinetics of water‐rock interactions , 1984 .
[23] R. Garrels. Montmorillonite/Illite Stability Diagrams , 1984 .
[24] P. Aagaard,et al. Activity/Composition Relations among Silicates and Aqueous Solutions: II. Chemical and Thermodynamic Consequences of Ideal Mixing of Atoms on Homological Sites in Montmorillonites, Illites, and Mixed-Layer Clays , 1983 .
[25] R. Lowson. Aqueous oxidation of pyrite by molecular oxygen , 1982 .
[26] R. Berner. Rate control of mineral dissolution under Earth surface conditions , 1978 .
[27] E. Brown. The greenschist facies in part of eastern Otago, New Zealand , 1967 .
[28] R. A. Yates,et al. Economic geology of New Zealand , 1967 .