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La presente investigación revela aspectos sobre los métodos geoquímicos aplicados a la exploración de depósitos minerales, como las aplicaciones prácticas e indicaciones sobre de las diversas técnicas empleadas en el campo y y laboratorio. La exploración química de los depósitos minerales como método de prospección, comprende la investigación e interpretación de anomalías químicas relacionadas a la mineralización dentro de varias sustancias naturales como rocas, aguas y vegetación para así localizar depósitos minerales ocultos. La naturaleza de estas anomalías se divide en dos grupos: las anomalías primarias formadas durante el periodo de mineralización y las secundarias, formadas por la destrucción y dispersión del depósito metalífero durante el ciclo de intemperismo y erosión. Sin embargo, existen algunas anomalías de naturaleza "residual" o "vestigial", las cuales son descubiertas mediante el muestreo sistemático de rocas o de los suelos que de ellas derivan. A esto se suma, la dispersión de elementos en solución puede dar origen a muchas variedades de anomalías secundarias que tienen importancia en la exploración geoquímica como las dispersiones secundarias en las aguas de fuentes, pozos y aguas corrientes, en las cajas de cuerpos mineralizados; en coberturas de carácter no residual sobre y cerca de depósitos mineralizados y aquellas dispersiones secundarias en vegetales. Paralelamente a esta exploración geoquímica, tenemos otras métodos comom los técnicas colorimétricas, basadas en reactivos que indican cambios de color y los de análisis espectográfico, que complementan paulatinamente dicho proceso minerológico.

Jul 20, 1956

By Evan C. Morgan G

El presente texto describe el panorama historiográfico de la mina de Condoroma, trabajos y el uso de los métodos de exploración realizados en dicha zona. Situada en el distrito de Condoroma, provincia de Espinar, Cusco, las minas de Condoroma fueron anteriormente trabajadas por los españoles, pero es a partir de 1927 y con la compañía Gibson que los trabajos mineros se reactualizan y se emplea la construcción de un tunel corta-veta de 170 metros de longitud, que al encontrarse con la veta, la extendió a 30 m. Posteriormente en 1952, se interesa la firma Mauricio Hochschild, suscribiendo un contrato de Opción por tres años con el Sr. Carlos Herrera Rozas. Firmada la Opción, se procedió primero a explorar las minas de Kata, por contener vetas vírgenes, y luego, las de Condoroma. Entre los métodos de exploración utilizados estaban los piques, las trincheras, la limpieza superficial con tractor, la perforación con diamantinas y la exploración geofísica. Finalmente, y tras haber desarrollado este programa de exploración con diamantinas, se pudo fijar los valores comerciales del yacimiento minero, aunque a un costo un tanto elevado. Empero la utilización de este moderno método de exploración, permitió revalorizar los yacimientos abandonados y colocarlos dentro de un espacio productivo.

Jul 20, 1956

By Vicente Martínez Guerra

Producto de una de las operaciones realizadas en la Cerro de Pasco Corporation, se obtienen algunos elementos y subproductos químicos como el arseniato de calcio que ocupa el primer lugar en ventas en dicha compañía. Por ello, el objeto del presente texto describe el proceso y el uso de As2 O3 para la fabricación del arseniato de calcio en la planta de fundición de La Oroya, como su aplicación de insecticidad mineral en la agricultura. Dentro de este periodo, el elemento químico será recuperado en el cottrell de arsémico, de los humos provenientes de los hornos tostadores de los minerales de cobre, precipitando una concentración oscilante entre 40 a 45% con un contenido de cobre de 4%. donde el polvo sufre una tostación para así concentrar el cobre por sublimación del arsénico. Asimismo en este sistema de fabricación de arseniato, la liberación del As2 O5 del piroarsenIato de calcio se realiza por ataque con ácido sulfúrico, garantizando la pureza de este óxido en la precipitación final del proceso. En consecuencia, la aplicación del arseniato de calcio, como insectida inorgánico mineral protege el sistema ecológico, dado su bajo contenido de arsénico soluble en agua, al tiempo que se ajusta a las reglamentos oficiale vigentes del país.

Jul 20, 1956

By Hernando Labarthe

"El siguiente texto describe la importancia de la actividad del Banco Minero en el Perú, a través de la instalación y operación de sus plantas de beneficios, como las ventajas, las instalaciones, organización y proyecciones futuras de dicha actividad. Dichas Plantas de beneficio inician sus actividades en la concentradora N°1 La Virreyna, extendiéndose posteriormente a 5 operadoras más como: Sacracancha, Huachocolpa, Dorado, Tonsuyoc, Huarochirí. De otro lado, el significado de la instalación y operación de estas manufacturas de beneficio supone un doble aporte a la minería, en el sentido que ayuda al minero en la inversión de sus utilidades -en tanto elimina el control de otras actividades en la operación-, como fomenta la producción a través del inicio de nuevas operaciones, incrementando las entradas fiscales. Por último, la sección Plantas de Beneficio del Banco Minero del Perú se encarga de la operación y control de las concentradoras, de los estudios, diseños y proyectos de nuevas plantas, del control de préstamos y habilitaciones a los minerosabastecedores. "

Jul 20, 1956

By Víctor R. Cabrera

Para un mayor avance en su producción, las minas de cielo abierto u "open it" de Marcona, utilizan unidades de mayor tamaño en el transporte, puesto que reduce el costo unitario del trabajo. En este aspecto, el objetivo del trabajo describe el uso de máquinas comprendidas para su uso, rendimiento de costo, pala, control de tiempo, tiempo de operaciones y el trabajo con traillas dentro de esta modalidad. etc. Como primer punto, las máquinas cargadoras, las palas mecánicas, etc, incrementan su tamaño constantemente y como tal, las operaciones de transporte cambiaron de uso de ferrocarril a de los camiones con 10,15, 20. 30 y 50 tonelajes por viaje. Posteriormente con el advenimiento de motores diesel, diseño, construcción, perforación y transporte de las máquinas cargadoras, se creó una minería de cielo abierto más económica, flexible y eficiente. En este punto, las operaciones estacionarias, sea con palas o las perforadoras de voladura, utilizaron preferiblemente la energía eléctrica que simplifica la operación y facilita el mantenimiento y las reparaciones. Mientras que las operaciones de perforación, voladura, carguío y acarreo se analiza las características de toneladas rotas por perforación, los cálculos de sobreperforación, los materiales explosivos usados, respectivamente. En cuanto la extracción de palas y volquetes, se evalúa la calidad del disparo, número de voloquetes, capacidad horaria. Finalmente en el trabajo con traillas, se evalúa la influencia del costo de las demoras relativas en las palas y los volquetes, pérdidas de la capacidad potencial de la pala cuando hay insuficiencia de volquetes, asi como las variaciones de la capacidad según la distancia de acarreo.

Jul 20, 1956

By Daniel Rodríguez Hoyle

El objeto de la siguiente investigación refiere los problemas encontrados en torno la propiedad minera y a la eficiencia de la Organización y Administración de esta industria en general. En este aspecto, se descubrieron diversos inconvenientes como: la titulación antigua, que dificulta la ubicación entre el campo y el relacionamiento en un plano de las concesiones del distrito minero en estudio, la no correspondencia entre el conjunto de conseciones con los sistemas geodésicos y topográficos de la Carta Nacional; el rebasamiento numérico de denuncios de los concesionarios ubicados en una superficie relativamente pequeña y la desmesurada labor de los concesionarios como del Estado por mantener en vigencia dichas conseciones. Por ello, se sugiere que el adecuado desarrollo del agrupamiento de concesiones mineras, como la inclusión de dicho procedimiento en la legislación minera y la designación de una comisión que evalué la inserción de esta agrupación a la legislación minera, soluciona los posibles problemas de propiedad.

Jul 20, 1956

By José Bellina E

"El propósito del siguiente estudio es mostrar el análisis comparativo de los reactivos de flotación de las distintas nacionalidades (americana, alemán, japonés)-en tanto herramienta de conocimiento y difusión- para el manejo de plantas metalúrgicas del país. Los factores a considerar en dicho estudio fueron: igualdad en factor molienda, densidad de pulpa, pH en el circuito, tiempo de flotación y prueba de paladas. Los reactivos utlizados son Xantato(Z-3), Xantato,(Z-4), Xantato(Z-5),Aeroflat 15, Aeroflat 25 y aceite de pino,respectivamente. Concluyendo que de cada reactivo estudiado, se compara su calidad como promotor y factor precio. Así para el XANTATO Z-3, el Xantato americano y alemán son de calidad semejante, con la variante que el alemán es un 22% más económico en su precio de compra. En cuanto al xantato japonés es de menor fuerza que los anteriores, siendo su precio más o menos igual al alemán. En el XANTATO Z-4, el xantato americano es de mejor calidad que los otros dos, aunque estos son también un 22% más económicos. Para el XANTATO Z-5, no hay casi diferencia entre el xantato alemán y el americano en cuanto a su calidad como promotor. El precio del xantato alemán es un 30% menor que el americano. En cuanto al xantato japonés es de menor fuerza que los anteriores, siendo su precio mayor que el xantato alemán. En el AEROFLOAT 15, es evidente que el aerofloat americano es mejor en calidad como promotor que los otros dos y su precio es casi similar al alemán. El japonés es inferior en calidad y su precio es similar a los otros. De otro lado, en el AEROFLOAT 25, el Aerofloat alemán da mejores resultados para esta flotación de cobre oxidado, donde su precio es similar al norteamericano. El japonés es inferior en calidad y su precio es también similar a los otros. Finalmente en el Aceite de pino, es indiscutible que el americano sea de mejor calidad que el alemán y japonés, sin diferencias destacables."

Jul 20, 1956

By E. B. Spice

Although much may be learned about the economics of cold weather operations by studying successful mining ventures in southern and central Canada, it is the purpose of this article to extend the study by considering only permafrost areas. Geographically this means most of the country north of the 60th parallel. In this area, at the present time, only five Canadian companies are carrying on routine and successful mining operations on a year-round basis. However, there have been some score of unsuccessful ventures, and a number of properties in the development stage show promise of being producers. Problems of cold weather are worthy of study. It may be pointed out that successful mines in this area face problems of isolation and costly transportation as well as cold weather. To reach valid conclusions, consider the development of a mythical mineral deposit located on the 65th parallel in the heart of the barren lands; problems of isolation and transportation will be ignored.

Jul 1, 1956

By Juan Rassmuss

El presente artículo señala el valor del azufre y la influencia del método de beneficio en lsu explotación. Asimismo, se describe los yacimientos de Piura y los de Báyovar, como del extremo norte está Ticsani, Tutupaca, Yucamani, Cano y en el Sur, Paucarany. La formación de estos yacimientos se debe a lla oxidación parcial de sulfuro de hidrógeno de origen volcánico, a excepción de los yacimientos de Bayovar y Piura, considerados como productos resuidual de petróleo.

Jul 1, 1956

By L. Bombardieri, H. F. Mills

Iron King mine, producing gold-silver-lead-zinc-ore, is 10 miles east of Prescott, Ariz. At present the 1806 level is being developed. The echelon pat tern of ore deposit continues at depth but is less pronounced, and the orebody is now more or less continuous over 2600 ft of strike length, with widths 5 ft to as high as 26 ft where overlapping of lenses occurs in one section of the mine. Better continuity of ore at depth has encouraged systematic mining and improved plant facilities to offset higher operating costs. With favorable persistence of ore at depth, the three-compartment No. 6 hoisting shaft appeared inadequate to handle increased tonnage from greater depths, and in 1952, a four-compartment steel and concrete shaft was started. This is now at a depth of 1906 ft, and shaft pockets and loading cartridges are being installed on the 1806 level. Ore from the new shaft, hoisted in 5 ½ -ton Jeto bottom dump skips, is dumped into a 500-ton shaft bin, from which it is fed to a 16x30-in. gyratory crusher and conveyed 415 ft through an undersurface concrete gallery to the secondary crusher and conveying system supplying the 900-ton mill. Lead, zinc, and pyrite concentrates are floated, and the flotation tailings are cyanided after desliming. Waste from the new shaft is dumped into a 250-ton surge bin, fed from this bin to a 24-in. conveyor, and discharged into the glory hole above the block cave. The new shaft is served by a double-drum 400-hp hoist used for ore and waste; the No. 6 shaft conveys men and material.

Jul 1, 1956

By Lloyd Williams, H. K. Gibbs, William L. Crentz, J. W. Miller

"Reserves This investigation shows that the Poplar Creek is the most important bed in Scott County from a production standpoint. Although the Poplar Creek bed contains the largest reserve, the Big Mary has a larger recoverable reserve. Estimates of reserves also have been made for the Pewee, Red Ash, Windrock, Upper Pioneer, Jellico, and White Oak beds.Known measured and indicated reserves of coal, based on a minimum bed thickness of 14 inches and on 1,800 short tons per acre-foot of coal in place, are estimated to be 143 million tons as of January 1, 1954. Of this total, 74 million tons is in beds 28 inches and more thick. Areas in each bed were omitted from the estimate because available data relative to the bed characteristics are too meager for making an estimate that conforms with the definitions of measured and indicated coal adopted for this study. Should future drilling or development prove reserves in these areas, such reserves should be added to the total estimated reserves.Recoverable reserves of coal are estimated in beds 28 inches and more thick. This thickness is about the minimum now being mined by hand loading onto conveyors in the Appalachian region. The weighted average recovery for all beds in Scott County, as determined by this investigation, is 52.4 percent. This percentage is based on the total thickness of coal in the bed (less partings three-eighths inch or more thick) rather than on the thickness of the coal mined. Based on the weighted average percentage of recovery for all beds in Scott County, the recoverable reserves of coal are estimated to be 39 million tons as of January 1, 1954.Coal Analyses Chemical analyses of coal samples taken for this study show that the coal in Scott County is of high-volatile a bituminous rank except the Upper Pioneer bed, which is shown to be high-volatile B bituminous. The Pewee bed shows typical low-sulfur characteristics. The high ash and sulfur in the Big Mary are characteristic of that bed. The Poplar Creek is moderately low in ash and sulfur in areas where there is no parting in the bed."

Jun 1, 1956

By D. A. Reynolds, R. G. Travis, James J. Dowd, R. F. Abernethy

"1. Reserve estimates have been made for eight coal beds in Monongalia County, W.Va., but only the Pittsburgh, Sewickley, and Upper Freeport beds are important at this time. The Pittsburgh, Sewickley, Waynesburg, and Upper Freeport beds contain the largest recoverable reserves.2. Known measured and indicated reserves in all beds, based on a minimum thickness of 14 inches and 1,800 short tons per acre-foot of coal in place, are estimated at 3,526 million tons as of January 1, 1954. Of this total, 3,294 mil¬lion tons is in beds 28 inches and more thick. Areas in each bed except the Pittsburgh were omitted from the estimate because available data relative to the bed characteristics are too meager for making an estimate that conforms with the definitions of measured and indicated coal adopted for this study. Should future drilling or development prove reserves in these areas, such reserves should be added to the total estimated reserves.3. Recoverable reserves of coal have been estimated in beds 28 inches and more thick. This thickness is about the minimum now being mined by hand loading onto conveyors in the Appalachian region. The weighted average recovery for all beds in Monongalia County, as determined by this investigation, is 47.9 percent. This percentage is based on the total thickness of coal (less partings three-eighths inch thick or more) in the bed rather than on the thickness of the coal mined. Based on the weighted average percentage of recovery for all beds in Monongalia County, the recoverable reserves are estimated at 1,577 million tons as of January 1, 1954.4. Monongalia County coals of the major producing beds are of high-volatile a bituminous rank.5. The Pittsburgh and Lower Freeport beds in this county yield coal that can be used as metallurgical coal, especially when blended with low-volatile coals. The Lower Freeport coal is coked singly and in beehive ovens, and makes good metallurgical coke.INTRODUCTIONThe investigation to evaluate the reserves of coking coal was planned to cover three phases: (1) Estimation of known measured and indicated recoverable reserves of all coking coal; (2) study of methods of upgrading marginal coals through effective preparation; and (3) study of carbonizing properties of coals and coal blends not now widely used for metallurgical coke making."

Jun 1, 1956

By William L. Lennemann

Chemistry of uranium with respect to its hydrometallurgical recovery from carnotite ores was investigated and well defined during the radium boom period between 1900 and 1920. Since that time, methods used to extract uranium from its ores have remained basically either acid leaching or sodium carbonate leaching. Until about 1950, the only practical methods known for achieving a better than 75 pct U2O3 concentrate from the leach liquors involved fundamental chemical techniques for either purifying a solution prior to the uranium precipitation, or refining a crude uranium concentrate that was produced by neutralizing a pregnant mill liquor.

Jun 1, 1956

By Patrick H. O’Neill

The Choco placers, mined continuously since the earliest expeditions of the Spanish conquistadors, were exploited by the Indians prior to the conquest. Platinum is found in varying percentages with gold throughout the Choco placers and is found in minor percentages in some placers in other parts of Colombia. The Choco Department is on the west coast of Colombia between the western range of the Andes and the Pacific Ocean and extends from the San Juan River north beyond Panama to the Caribbean. The first reference in European literature to platinum was by Julius Caesar Scaliger in 1557. He did not assign any name to it but referred to it as an infusible metal found in the mines in the New World. The Spaniards had given it the name platina, which is the diminutive for plata, the Spanish word for silver. Don Antonio de Ulloa first recorded the name while on an official visit to the Choco from Spain in 1735.

May 1, 1956

By J. L. Humphrey

The origin of roof bolting is obscure, but is believed to have begun some 40 years ago in the mines of St. Joseph Lead Co. in southern Missouri. It was not until after World War II, and more particularly after 1949, as a result of the concentrated effort of the USBM, that roof bolting attracted widespread interest. It is estimated that at the end of 1954, 26 pct of all bituminous coal mining in the U. S. was being done under roof bolts. Those mines alone use nearly 2,000,000 roof bolts per month, according to USBM statistics. Uses in metal mines are increasing rapidly, as confidence and knowledge grow. The application has found equal success in other fields, such as tunneling work for dam and waterway construction and right of way maintenance on highways and railroads.

May 1, 1956

By Richard Lewis

"El presente artículo describe la geología del yacimiento cobre-plomo-zinc de Quiruvilca, ubicada en el Departamento de La Lilbertad, Perú. Esta es la única mina más grande de la región y pertenece a la Northern Peru Mining and Smelting Co. Los yacimientos de este distrito son meso y epitermales y se formaron por rellenos de fisuras. La mineralización siguió un sistema preexistente de fracturas de tensión y corte y las vetas forman un sistema bien definido de enrejado oblícuo. Solo algunas de las vetas en la región son productivas."

May 1, 1956

By J. L. Gillson

The big mass of anorthosite in the Lake Sanford district and the bodies of titaniferous magnetite that occur in a small area near the south margin of the mass have been described repeatedly, and the puzzling problems of the genesis of the rocks and ores have stimulated the deductive reasoning of geologists for a hundred years. Some of these men have taken a leading part in describing the anorthosite rock and forming hypotheses concerning its origin; some have contributed most to the study of the ore deposits; and some have made classical Studies introducing a basic approach to the problems of the anorthosite rock and genesis of the titaniferous magnetites. Much of the writing on the problems of rock and ore genesis has been based on physical-chemical reasoning rather than on field and microscope observations of the rocks and ores. Most of these geologists conclude that the anorthosite was formed by true magmatic crystallization, involving previous settling or squeezing out of ferromagnesian minerals from the parent magma. The associated gabbro is a separate segregation or later intrusion, and the lighter colored and finer grained facies of the anorthosite is either a chilled border zone of the anorthosite or the result of granulation by crushing of the coarse, dark blue rock of the main mass. This blue rock, called the Marcy type, is named after the highest peak in the range. The finer grained and lighter colored rock is called the Whiteface, after another mountain appropriately named for a cliff colored by this facies of the anorthosite.

Mar 1, 1956

By John Gittins

Lots 11 and 12, Range IX, Calumet island, are underlain by a Grenville metamorphic complex into which sills of tourmaline granite pegmatite have been injected. The pegmatite has an average mode-potash feldspar 65 per cent, sodic plagicdase 10 to 20 per cent, quartz 5 to 20 per cent, tourmaline 10 to 15 per cent, accessory minerals < 5 per cent; it is unzoned except for a narrow border zone. Some of the feldspar has been replaced by calcite. Microcline has been ?partially replaced by sodic plagioclase. Three varieties of tourmaline are present (black, blue, and green) and spectrographic analysis suggests progressive compositional changes during its crystallization. The presence of U- and Th-bearing minerals in the pegmatite prompted the Quebec Nickel Cor,porat10n, Ltd., to explore the possibility of developing the pegmatite but it does not appear that this is economically possible at the ? present time. Tt\e Grenville metamorphic complex consists of recrystallized limestones and calcsilicate rocks of the albite-epidoteamphibolite facies and the amphibolite facies, which were derived from sedimentary rocks. Several of these are dis-equilibrium assemblages, and retrograde metamorphism has probably formed biotite and epidote from hornblende. The schistosity of the gneisses dips steeply eastward. Numerous strike faults are roughly parallel to the schistosity and one of the pegmatite sills is bounded by such a fault, dipping at 60 ° with about one foot of fault breccia. The general structure of the map-area seems to be an asymmetrical syncline ?overturned to the west. The emplacement of the pegmatite is associated with a period of folding, metamorphism, and igneous intrusion.

Jan 1, 1956

By John R. Reynolds

This paper describes mining and milling methods of the American Smelting & Refining Co. at the Morning mine in the Mullan area of the Coeur d&apos;Alene mining region in Idaho and is one of a series of Bureau of Mines reports dealing with methods and costs of mining throughout the United States. The Morning mine has been described previously in a Bureau of Mines report published in 1930,2/ and the milling methods and costs at the Morning concentrator were presented in a Bureau of Mines report published in 1932. 3/ These reports are supplemented by this publication, which presents data to show the effect of changing times and conditions on a typical medium-size mining operation during the latter part of its history, when costs were rising and production was from increasingly greater depths. The report contrasts two periods in the history of the mine-periods not too far separated in years but considerably different in economic conditions. During the first period (1939) costs of labor and materials were moderate, mining operations were just being transferred from the main shaft to deeper workings opened from the offset shaft, and the operation prospered. During the second period (12 years later) production costs had increased following the national trend in all industry, mining was from greater depths near the bottom of the ore body, and the operation was becoming unprofitable. Mining on the lower levels of the property ceased in 1953.

Jan 1, 1956

By Paul Meadows

The Buckrange reservoir, Stephens field, Ark., is approaching the economic limit of production under present operating conditions. Over 100 million barrels of oil remaining in the reservoir will not be recovered by primary producing methods. The Bureau of Mines, in cooperation with the Arkansas Oil and Gas Com-mission, made the petroleum-engineering study presented in this report to aid operators in evaluating secondary-recovery possibilities in the reservoir and in planning secondary-recovery programs if their initiation is decided. The Stephens field, in Columbia, Nevada, and Ouachita Counties, Ark., is about 12 miles northeast of Magnolia, Ark., and 15 miles west of the Smackover field. Surface elevations in the area average about 240 feet above sea level.

Jan 1, 1956