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![](./images/clear.gif) 1.- Copper-excess stannoidite and tennantite-tetrahedrite as proxies for hydrothermal fluid evolution in a zoned Cordilleran base metal district, Morococha, central Peru
Mineralogical Association of Canada; Ottawa, ON; CAN; Canada, 2012
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![](./images/clear.gif) 2.- Fluid evolution in Cordilleran polymetallic veins; insights from microthermometry and LA-ICP-MS of fluid inclusions
University of Szeged, Department of Mineralogy, Geochemistry and Petrology; Szeged; HUN; Hungary, 2010
IMA2010; 20th general meeting of the International Mineralogical Association; abstracts
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![](./images/clear.gif) 3.- Fluid evolution in zoned cordilleran polymetallic veins; insights from microthermometry and LA-ICP-MS of fluid inclusions
Elsevier; Amsterdam; NLD; Netherlands, 2011
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