Reverse Osmosis contributing to metal zoning in porphyry type deposits: A case study
Representing the main source of copper in the world, porphyry copper deposits have been widely studied. Different models have tried to explain the observed metal zoning, but they did not completely explain it. A Permian Cu-Mo porphyry deposit in the San Rafael Massif in Argentina shows a similar met...
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Acceso en línea: | https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_01691368_v71_n_p191_Japas http://hdl.handle.net/20.500.12110/paper_01691368_v71_n_p191_Japas |
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paper:paper_01691368_v71_n_p191_Japas2023-06-08T15:18:15Z Reverse Osmosis contributing to metal zoning in porphyry type deposits: A case study Infiernillo porphyry deposit Osmotic differentiation Potential-energy gradients Pressure-sensitive process Copper deposits Deposits Metals Molecular physics Molybdenum Osmosis Potential energy Reverse osmosis Zoning Argentina Cooling model Halo formation Natural minerals Permian Porphyry copper deposits Porphyry deposits Pressure sensitive Copper copper molybdenum ore deposit osmosis Permian porphyry pressure effect zoning Argentina Mendoza San Rafael Massif Representing the main source of copper in the world, porphyry copper deposits have been widely studied. Different models have tried to explain the observed metal zoning, but they did not completely explain it. A Permian Cu-Mo porphyry deposit in the San Rafael Massif in Argentina shows a similar metal zoning pattern to those described elsewhere. However, some particular features depart from the conventional cooling model. Based on data from this deposit and on theoretical background, we present and discuss Reverse Osmosis as a complementary process which could have contributed to porphyry metal zoning during the phyllic stage. The existence of potential-energy gradients and the different relative rejection values for distinct ions make Reverse Osmosis a natural mineral-concentration process. At temperatures corresponding to those of porphyry phyllic halo formation and in presence of a phyllic (clay) membrane, Cu, Ag, Zn and Pb would show a strong osmotic differentiation that could have led to the observed metal zoning. © 2015 Elsevier B.V. 2015 https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_01691368_v71_n_p191_Japas http://hdl.handle.net/20.500.12110/paper_01691368_v71_n_p191_Japas |
institution |
Universidad de Buenos Aires |
institution_str |
I-28 |
repository_str |
R-134 |
collection |
Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) |
topic |
Infiernillo porphyry deposit Osmotic differentiation Potential-energy gradients Pressure-sensitive process Copper deposits Deposits Metals Molecular physics Molybdenum Osmosis Potential energy Reverse osmosis Zoning Argentina Cooling model Halo formation Natural minerals Permian Porphyry copper deposits Porphyry deposits Pressure sensitive Copper copper molybdenum ore deposit osmosis Permian porphyry pressure effect zoning Argentina Mendoza San Rafael Massif |
spellingShingle |
Infiernillo porphyry deposit Osmotic differentiation Potential-energy gradients Pressure-sensitive process Copper deposits Deposits Metals Molecular physics Molybdenum Osmosis Potential energy Reverse osmosis Zoning Argentina Cooling model Halo formation Natural minerals Permian Porphyry copper deposits Porphyry deposits Pressure sensitive Copper copper molybdenum ore deposit osmosis Permian porphyry pressure effect zoning Argentina Mendoza San Rafael Massif Reverse Osmosis contributing to metal zoning in porphyry type deposits: A case study |
topic_facet |
Infiernillo porphyry deposit Osmotic differentiation Potential-energy gradients Pressure-sensitive process Copper deposits Deposits Metals Molecular physics Molybdenum Osmosis Potential energy Reverse osmosis Zoning Argentina Cooling model Halo formation Natural minerals Permian Porphyry copper deposits Porphyry deposits Pressure sensitive Copper copper molybdenum ore deposit osmosis Permian porphyry pressure effect zoning Argentina Mendoza San Rafael Massif |
description |
Representing the main source of copper in the world, porphyry copper deposits have been widely studied. Different models have tried to explain the observed metal zoning, but they did not completely explain it. A Permian Cu-Mo porphyry deposit in the San Rafael Massif in Argentina shows a similar metal zoning pattern to those described elsewhere. However, some particular features depart from the conventional cooling model. Based on data from this deposit and on theoretical background, we present and discuss Reverse Osmosis as a complementary process which could have contributed to porphyry metal zoning during the phyllic stage. The existence of potential-energy gradients and the different relative rejection values for distinct ions make Reverse Osmosis a natural mineral-concentration process. At temperatures corresponding to those of porphyry phyllic halo formation and in presence of a phyllic (clay) membrane, Cu, Ag, Zn and Pb would show a strong osmotic differentiation that could have led to the observed metal zoning. © 2015 Elsevier B.V. |
title |
Reverse Osmosis contributing to metal zoning in porphyry type deposits: A case study |
title_short |
Reverse Osmosis contributing to metal zoning in porphyry type deposits: A case study |
title_full |
Reverse Osmosis contributing to metal zoning in porphyry type deposits: A case study |
title_fullStr |
Reverse Osmosis contributing to metal zoning in porphyry type deposits: A case study |
title_full_unstemmed |
Reverse Osmosis contributing to metal zoning in porphyry type deposits: A case study |
title_sort |
reverse osmosis contributing to metal zoning in porphyry type deposits: a case study |
publishDate |
2015 |
url |
https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_01691368_v71_n_p191_Japas http://hdl.handle.net/20.500.12110/paper_01691368_v71_n_p191_Japas |
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1768542500862033920 |