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PROFIL D'ENTREPRISE Léandre Gervais & Associé(e)s est une société d'experts-conseils en ingénierie de la structure, de la mécanique & de la tuyauterie, et de l'électricité et de l'instrumentation. Nous offrons des services hautement spécialisés à notre clientèle des secteurs industriels des mines et de la métallurgie, au Québec, au Canada ainsi que dans plusieurs autres pays du monde. Notre mission est d'assurer à nos clients un ensemble de services d'ingénierie de haute qualité contribuant à la mise en oeuvre et à la réalisation de leurs projets d'affaires. Léandre Gervais & Associé(e)s emploie 36 employés à temps pleins et opère à partir de Val-d'Or, province de Québec. SERVICES OFFERTS Nous avons réalisé de multiples mandats pour notre clientèle de différent pays du monde dans les domaines d'expertise les plus variés : ?Études de faisabilité ; ?Ingénierie conceptuelle ; ?Ingénierie de détail ; ?Gestion de projets ; ?Ré-ingénierie de la maintenance.

May 1, 2001

By Stefan Planeta

On discute les performances techniques et économiques des méthodes d'exploitation à haut rendement dans les mines métallifères au Canada. L'accent est mis sur la dilution et pertes des réserves minières et sur les coûts opératoires et totaux. Une analyse technique de quelques opérations minières est également effectuée. Il ressort de cette analyse que les résultats réels des opérations minières en cours diffèrent souvent de ces planifiés suite à la dilution du minerai et aux pertes importantes des réserves minières. On propose, définit et discute un certain nombre des facteurs de performances technologiques et économiques pour pouvoir mieux apprécier les problèmes rencontrés dans plusieurs mines en opération. À l'aide des études de cas on démontre impact négatif de la dilution et des pertes additionnelles des réserves minières sur la rentabilité des opérations en cours et sur les nouveaux projets miniers. On conclut, que l'application des indicateurs proposés donnerait un outil valable, aux opérateurs miniers, aux niveaux de la planification, du suivi des travaux d'exploitation et d'éventuelles études comparatives entre les différentes situations minières. ABSTRACT The paper discusses technical and cost performance of bulk mining methods in Canadian U/G metal mines. It focuses on ore dilution, ore reserves losses as well as on operational and total cost. Technical analysis of some mining operations has been performed. It indicates that due to dilution and significant reserves losses, the actual results of mining operations often differ substantially from those planned. The paper proposes, defines and discusses several indicators quantifying technical and economical performance in order to assess better the problems encountered in several operating mines. The case studies presented here have demonstrated an adverse effect of dilution and additional reserves losses onto profitability of existing operations and new mining projects. It is concluded that the application of the above mentioned indicators may be beneficial for mine operators. They may become a very useful tool at the stages of planning, follow-up of mining works and with regards to comparative studies between different mining situations.

May 1, 2001

By Joseph W. Ruetz

The paper describes the San Nicolas deposit, México. San Nicolás deposit is the most important VMS deposit discovered in Mexico to date, and a major deposit on a global scale. The discovery of San Nicolas resulted from the early recognition of VMS mineralization in a region not known for this style of mineralization, and the flexible use of appropriate exploration technology.

Apr 24, 2001

By Francisco Camus

"El presente trabajo describe la geología y mineralización del proyecto minero Los Chankas. Dicho yacimiento está ubicado en la parte oeste de la Cordillera Central de los Andes del sur del Perú, dentro de la provincia metalogenética de Andahuaylas-Yauri, como un sistema porfirítico asociado a ambientes cordilleranos. El depósito está relacionado a un complejo de intrusiones félsicas y desarrollo de fases orto-tardi magmáticas e hidrotermales como procesos formadores de a mineralización económica del tipo Cu-Mo-Au. Las diferentes zonas de mineralización muestran partes superiores con pitch limonita, neotocita goetita y esporádicamente tenorita y ferromolibdenita. La zona de enriquecimiento muestra calcocina, covelina, digenita y bornita, con ocurrencia de calcopirita, bornita y molibdenita en la zona de sulfuros primarios. Las características conocidas de mineralización en Los Chancas definen un sistema porfirítico de niveles de emplazamiento relativamente profundos, con evidencias de particularidades metalogenéticas, las cuales son estudiadas como parte de la evaluación del proyecto."

Apr 24, 2001

By Patrick High Smith

The paper summarizes the results from geochemical orientation and project surveys in North and South America. The orientation surveys were designed to characterize the soil gas response over buried mineralization and compare soil gas geochemistry with other geochemical exploration techniques for overburden. In addition to successful tests in orientation surveys, soil gas geochemistry has been applied in large-scale exploration programs for gold, copper, and zinc. The studies includes results from several of these surveys, including the Crandon Zn-Cu massive sulfide deposit in Wisconsin, USA, and the Ruby Star skarn Cu deposit in Arizona, USA.

Apr 24, 2001

By Richard Zamora

El presente trabajo describe la mineralización del fierro, cobre y oro en el distrito de Montaverde, Chile. El distrito Mantoverde está ubicado a 53 km al SE del puerto de Chañaral en la Cordillera de la Costa de la III Región de Atacama, Chile. La explotación minera del distrito se inició a principios del siglo pasado y continuó en forma irregular hasta que en 1989 la Empresa Minera de Mantos Blancos S.A. desarrolló los trabajos de exploración. Posteriormente, dichos trabajos a escala distrital permitieron ampliar el conocimiento de la mineralización hipógena e incrementar el potencial del yacimiento. En este sentido, el presente texto señala diversos antecedentes que ubican a Mantoverde como uno de los más importantes distritos cupríferos de la Cordillera de la Costa de Chile.

Apr 24, 2001

By Peter Megaw

The paper point out that the carbonate Carbonate Replacement Deposits (CRDs) are epigenetic, intrusion-related, high-temperature sulfide-dominant Pb-Zn-Ag-Cu-Au-rich deposits that typically form lenses or elongate to elongate-tabular bodies referred to as mantos or chimneys. Recent studies have shown that CRDs do occur in predictable geologic environments, allowing focusing of regional exploration. In addition, they have mappable alteration patterns that can be used to determine the magnitude of a given system and elemental zoning patterns that greatly enhance the chances of drilling success. Several recent discoveries of “blind” replacement deposits have been made by careful field evaluation of host and capping rocks coupled with geophysics.

Apr 24, 2001

By Jan Klein

"The last decade of the 20th century saw the development of one of the last missing geophysical tools for mineral exploration: the Airborne Gravity Gradiometer. It is possible that Airborne Induced Polarization, one of the stillelusive systems, will make its debut in the next few years. In this sense, the paper point out are the most recent and important improvements in geophysical technologies for mineral exploration. Airborne techniques are followed by the systems used on the ground and in boreholes. New equipment and data processing and modeling software are referred to. Brief remarks are made about developments that can be expected in the years to come, these will be mainly focussing on deep search in rugged and conductive terrains. "

Apr 24, 2001

By Jeffrey Hedenquist

The Lepanto and Victoria epithermal deposits contain in excess of 8 Moz Au, associated with massive enargite-cemented breccia and quartz-carbonate-base metal veins, respectively. The two deposits are separated by 500 m, but the latter was not discovered until the former was nearly mined out. The sulfid assemblages of these adjacent deposits are characterized by high- and intermediate-sulfidation states, respectively. However, gold was introduced after enargite at Lepanto, associated with an assemblage that is similar to that of the Victoria ore. An even larger gold resource is present in similar to that of the Victoria ore. An even larger gold resource is present in the Far Southeast porphyry Cu-Au deposit, the top of which lies 200-400 m beneath and adjacent to these two epithermal deposits.

Apr 24, 2001

By Patricio Jones

Veladero es un depósito epitermal de metales preciosos de alta sulfuración hospedado en brechas y rocas de litologías brechadas y está situado en San Juan, Argentina. Regionalmente, se localiza en el cinturón volcánico terciario del Valle del Cura (Argentina), que es adyacente al cinturón de El Indio (Chile). En ese sentido, el presente texto describe los factores que descubrieron el depósito, menciona las principales referencias respecto de su geología local y regional y enfatiza los aspectos institucionales y técnicos del descubrimiento, realizado por Minera Argentina Gold S.A. (MAGSA).

Apr 24, 2001

By Xuejing Xie

Exploration geochemistry for many years has been very effective in searching for mineral deposits covered by residual overburden or blind ore bodies hosted in pre-ore rocks. It has not been as effective discovering ore bodies deeply concealed under various kinds of transported overburden or post-ore sedimentary and volcanic rocks. From the 1980s to 1990s, various types of new geochemical techniques with the ability of deep-penetration through exotic covers have been developed. The concepts and methodology of deeppenetrating geochemistry are evolving from partial extraction and gas surveys prevailing from the 1950s up to now, but there are intrinsic differences. Most of the new deep-penetrating methods are used in detailed surveys to delineate deeply concealed ore bodies which could not be ascertained by conventional geological, geophysical and geochemical surveys. In this sense, the sampling and analytical methods of Nameg and Momeo are described briefly. Experiments of such strategic deep-penetrating geochemical surveys have been carried out in desert, alluvium, steppe and laterite covered terrains in China, Australia and Uzbekstan.

Apr 24, 2001

By Douglas Silver

During the past decade, Latin America has commanded an ever growing percentage of the world’s mineral exploration expenditures. Today, it controls approximately 30%. This has led to an increased number of large and small mineral discoveries over prior years for a variety of metals and the construction of many new mines. Its dominance is also seen in the larger than expected share of international mining capital investment. This has given its workers a competitive edge in global terms and an expertise that will ensure a long-term longevity to its mining industry. The best incentive for making vestment decisions is success. In this regard, Latin America’s success has compounded the incentives for further investment. Despite the large amount of foreign investment in Latin America, the wealth of these nations is not merely in its geological potential. The reason that several Latin American countries rank as global leaders in metal production is strongly influenced by their development of a strong mining culture, a culture which has been cultivated over many centuries. Good business practices provide another strong attraction to these regions. Additionally, Latin Americans have strong scientific and technical expertises. This is seen both in the investments’ size and the preference for high domestic employment. Relative to the number of domestic miners, the number of expatriates operating in Latin America is only a token few. In essence, the world markets are investing into the local geology and people.

Apr 24, 2001

By Marcelo Claure

"La evolución de los Andes Bolivianos ha estado dominada por arcos magmáticos donde existe una progresiva migración hacia el oeste y que están relacionados a procesos de subducción. El arco volcánico moderno se inicióhacia los 26 Ma debido a la subducción de la placa de Farallón y subsecuente aumento en la velocidad de convergencia. Asimismo, la región de la Cordillera Occidental desarrolló campañas de exploración que condujeron al descubrimiento de numerosas zonas mineralizadas y prospectos de interés económico, debido a las favorables condiciones geológicas para el descubrimiento de diferentes tipos de yacimientos ya sean diseminados, en stockworks o filonianos, con mineralización de plata, oro, plomo, cadmio, indio y germanio, entre otros. En este sentido, el presente texto señala los resultados de esta exploración, los ciclos evolutivos, su cronología absoluta, los rasgos geoquímicos y potencial minero de la región andina. "

Apr 24, 2001

By Lluis F. Fontboté

The paper point out the deposits about the carbonate-hosted San Gregorio Colquijirca, as products of an epithermal high sulfidation system. Field, geochemical, and geochronological evidences suggest that the different ore types of the Colquijirca District are caused by a pulsed high sulfidation system subsequent to the emplacement of a diatreme volcanic complex. The first stage formed disseminated Au±Ag mineralization in areas affected by vuggy quartz alteration at Marcapunta. During a second stage, base metal mineralization replaced Eocene carbonate sediments from the Marcapunta diatreme to 2.5 km more to the north. San Gregorio and Colquijirca are to our knowledge the first "carbonate-hosted epithermal Zn-Pb high sulfidation deposit" recognized as such. The correct recognition of this ore type opens new exploration possibilities for base metal in high sulfidation systems affecting carbonate rocks.

Apr 24, 2001

By Larry Meinert

Most large skarn deposits are zoned in both space and time relative to associated intrusions, and this zonation can be used to guide exploration. Zonation occurs on scales from km to, and reflects infiltrative fluid flow, wallrock reaction, temperature variations, and fluid mixing. In most skarn systems, there is a general zonation pattern of proximal garnet, distal pyroxene, and vesuvianite (or a pyroxenoid such as wollastonite, bustamite, or rhodonite) at the marble front. In addition, individual skarn minerals may display systematic color or compositional variations within the larger zonation pattern. Such patterns are reviewed for several well-studied examples of Cu, W, Au, and Zn-Pb-Ag skarns. In addition, many deposits have endoskarn or other alteration of the associated intrusion and recrystallization or other subtle changes in the surrounding wallrocks.

Apr 24, 2001

By Greg Corbett

The paper point out the styles of Pacific Rim epithermal gold mineralization. Some characteristics of differing styles of epithermal gold mineralization influence investment decisions (metallurgy, metal ratios, mining style), while others should be taken into account during prospecting (pyrite content and resistivity govern geophysical techniques, vein/breccia styles control drilling, gold distribution influences ore reserve determinations). Two groups of epithermal deposits are distinguished by the fluid style which controls ore and gangue mineralogy. High sulfidation systems develop from the reaction of hot acidic magmatic fluids with host rocks to produce characteristic zoned alteration and later sulfide (dominantly enargite-pyrite) and Au-Ag-Cu deposition. Ore systems display permeably controls governed by lithology, structure and breccias, typically phreatomagmatic breccia pipes, and should be distinguished from a group of generally non-economic acidic alteration including: steam heated alteration, lithocaps or barren shoulders, acid sulfate, and magmatic solfatara alteration.

Apr 24, 2001

By Luis Quevedo

En el proyecto Pangui, localizado al sureste del Ecuador de las provincias de Morona Santiago y Zamora Chinchipe, se descubrió un cinturón de pórfidos de cobre con tendencia N-S y un skarn de cobre. Esta zona se localiza entre el flanco occidental de la Cordillera del Cóndor y las estribaciones orientales de la cordillera real cercanas al borde limítrofe con el Perú. La mayor parte del área está cubierta por selva y las pendientes son abruptas. En la zona no hay una buena infraestructura de carreteras. En este sentido, el presente texto describe las actividades de Gencor y Billiton durante 6 años, así como los resultados de un año de actividades de Corriente/Lowell en los proyectos Warintza, Mirador y Panantza.

Apr 24, 2001

By Rita Pinto

El presente texto señala la mineralización en la zona de sulfuros de la Minera Yanacocha. Dicha minera está constituida por Newmont Mining Company, Compañía de Minas Buenaventura S.A. (44%) y la International Finance Corporation (5%) y es el más grande productor de oro, el cual se extrae por métodos de minado a cielo abierto y tratamiento por lixiviación. Asimismo en el área de Cerro Yanacocha se presentan las típicas alteraciones de un sistema hidrotermal de alta sulfuración emplazado dentro de brechas freatomagmáticas y rocas piroclásticas. Los minerales que se presentan están albergados principalmente en la zona de mixtos y sulfuros. y se encuentran en un orden de abundancia: calcosita, covelita y cuprita asociados a remanentes primarios de enargita, covelita.

Apr 24, 2001

By Raymond Jannas

El presente trabajo señala ejemplos de hallazgo de los depósitos de oro de alta calidad, enfatizando en las herramientas de uso de los geólogos para encontrar un yacimiento de impacto económico en Sudamérica. La competitividad en la búsqueda de nuevos depósitos minerales de oro de alta calidad conlleva una instrucción permanente en el tema. Por ello, es fundamental el uso de la información disponible para ser más selectivo y predictivo en la exploración. En ese sentido, el éxito en el hallazgo de yacimientos de calidad no se limita al conocimiento de los mejores depósitos, sino es importante es conocer y entender las características geológico-técnico-financieras que conforman un depósito de excepción.

Apr 24, 2001

By John Guilbert

"The paper examine the remarkable improvements in our understanding of the linkages among hydrothermal ore deposit types that are developing as we enter the 21st century. Dramatic changes have occurred in ourperceptions of formative processes and genetic models for hydrothermal deposits in the last 30 years that will profoundly change the techniques and methods whereby exploration for those deposits will proceed in the next decades. "

Apr 24, 2001