Kaolinite dissolution rates in batch experiments at room temperature and pressure: reply to ''on the interpretation of closed system mineral dissolution experiments,'' comment by Eric H. Oelkers, Jacques Schott, and Jean-Luc Devidal

By Huertas F.J.   Chou L.   Wollast R.  

Geochimica et Cosmochimica Acta, Vol. 65, Iss. 23, 2001-12 ,pp. : 4433-4434

Elsevier

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Mechanism, rates, and consequences of basaltic glass dissolution: II. An experimental study of the dissolution rates of basaltic glass as a function of pH and temperature

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Geochimica et Cosmochimica Acta, Vol. 67, Iss. 20, 2003-10 ,pp. : 3817-3832

Elsevier

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Interferometric study of the dolomite dissolution: a new conceptual model for mineral dissolution

By Lttge A.   Winkler U.   Lasaga A.C.  

Geochimica et Cosmochimica Acta, Vol. 67, Iss. 6, 2003-03 ,pp. : 1099-1116

Elsevier

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The effect of pH and temperature on kaolinite dissolution rate under acidic conditions

By Cama J.   Metz V.   Ganor J.  

Geochimica et Cosmochimica Acta, Vol. 66, Iss. 22, 2002-11 ,pp. : 3913-3926

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Comment on the paper by Pandalai et al.: Dissolution channels in quartz and the role of pressure changes in gold and sulfide deposition in the Archean, greenstone-hosted Hutti gold deposit, Karnataka, India (Miner Deposita 38:597–624)

By Kolb Jochen   Rogers Amanda   Meyer F.  

Mineralium Deposita, Vol. 39, Iss. 1, 2004-01 ,pp. : 114-116

Springer Publishing Company

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