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![](./images/clear.gif) 1.- ANALYSIS OF EVAPORATE MOUNDS AS A COMPLEMENT TO FLUID-INCLUSION THERMOMETRIC DATA; CASE STUDIES FROM GRANITIC ENVIRONMENTS IN NOVA SCOTIA AND PERU
MINERALOGICAL ASSOCIATION OF CANADA; OTTAWA, ON; CAN; CANADA, 2004
PACROFI VIII
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![](./images/clear.gif) 2.- DELAYED INCEPTION OF ORE DEPOSITION IN MAJOR LITHOPHILE-METAL VEIN SYSTEMS; THE SAN RAFAEL TIN AND PASTO BUENO TUNGSTEN DEPOSITS, PERU
GEOLOGICAL SOCIETY OF AMERICA (GSA); BOULDER, CO; USA; UNITED STATES, 2000
GEOLOGICAL SOCIETY OF AMERICA, 2000 ANNUAL MEETING
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![](./images/clear.gif) 3.- FE-TI-P OXIDE MELTS GENERATED THROUGH MAGMA MIXING IN THE ANTAUTA SUBVOLCANIC CENTER, PERU; IMPLICATIONS FOR THE ORIGIN OF NELSONITE AND IRON OXIDE-DOMINATED HYDROTHERMAL DEPOSITS
ECONOMIC GEOLOGY PUBLISHING COMPANY; LANCASTER, PA; USA; UNITED STATES, 2004
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![](./images/clear.gif) 4.- GENESIS OF THE GIANT, BONANZA SAN RAFAEL LODE TIN DEPOSIT, PERU; ORIGIN AND SIGNIFICANCE OF PERVASIVE ALTERATION
ECONOMIC GEOLOGY PUBLISHING COMPANY; LANCASTER, PA; USA; UNITED STATES, 2002
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![](./images/clear.gif) 5.- THE MINASTIRA PERALUMINOUS GRANITE, PUNO, SOUTHEASTERN PERU; A QUENCHED, HYPABYSSAL INTRUSION RECORDING MAGMA COMMINGLING AND MIXING
MINERALOGICAL SOCIETY; LONDON; GBR; UNITED KINGDOM, 1997
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