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Major Francis Hamilton Buchanan coined the term `laterite' (Latin; brick-rock) in 1807 for the red earths used for building blocks in southern India. Although these earths were actually weathered basalts, the term is now applied to weathering profiles developed upon a wide range of bedrocks. The Ni-laterites are a special class within the broad laterite family.

Jan 1, 1996

By V. McLemore, N. Dunbar, K. Donahue

There are three principle lines of evidence that indicate the clay minerals found in the Goathill North (GHN) rock pile at the Molycorp mine are predominantly a product of hydrothermal alteration, not weathering. The unweathered drill core and samples from GHN have similar types and abundances of clay-mineral groups based on XRD analysis. Chemical analyses from the electron microprobe reveal similar chemical compositions for the hydrothermal alteration clays in drill-core samples and clays found in the rock pile. Textural evidence gathered from petrographic and microprobe examination also suggests a hydrothermal origin for clay minerals.

Jan 1, 2007

By A. E. Wraith, J. Protheroe Jones, P. J. Mackey

The world’s first copper electrorefinery started production in 1869 at Burry Port in South Wales. Built within the Pembrey Copper Works which had commenced smelting operations in 1849, the new refinery was based on principles described in the British patents issued to J.B. Elkington in 1865 and 1869. Refining principles and practices pioneered there were key to the foundation of modern electro-refining practice in what is now a dominant international industry producing over 16 Mt of electrical grade copper annually. This paper explores the background to this pioneering application of the new, early 19th century, science of “electro-metallurgy” and examines its links to the contemporary decorative electro-plating industry and to the shortcomings of 19th century fire refining. The beginnings and early years of the Pembrey electrorefinery are briefly discussed in relation to the quality, applications and pyrometallurgy of copper at the time. More than a decade would elapse before the birth of the electrical age: the Pembrey refinery may be seen as one of its vital precursors. Note: This paper was originally published as part of the Copper 2013 proceedings (A.E. Wraith, P.J. Mackey and J. (formerly R.) Protheroe Jones, “Origins of Electrorefining: Birth of the Technology and the World’s First Commercial Electro-Refinery”, paper in Electrorefining, Vol. V, Book 2, (Eds. R. Abel and C. Delgado), Cu 2013 International Conference, pp. 19-33, IIMCh, Santiago, Chile, 2013). It is reproduced here together with a new Appendix and supporting references that lists the year of commencement of the first electrolytic copper refinery by country, 1869 to 1956. It all, the year of the first electrolytic copper refinery established for 15 countries is included. These 15 countries now produce more that 70% of world refined copper (for 2018). INTRODUCTION In the 1840s, the new science of ‘electro-metallurgy’, a term coined by Smee in 1841 (Smee, 1841), was being adapted to the decorative electro-deposition of silver in a thin, bright adherent coating that was evidently equal in appearance to traditional silverware (Williams, 1976). Chief among innovative manufacturers of decorative objects who took up the new art of silver electro-plating was the acclaimed firm of G.R. Elkington and Co. of Birmingham, England. The company, which vigorously developed all aspects of electro-metallurgy for the decorative trade, entered the field of ‘electrotyping’, a technique in which the surface features of a mould are copied on an electro-deposited copper layer which, when stripped off, can be used to reproduce an imprint of the mould. In essence, it is a form of casting by electrodeposition, invented in 1837 independently by Jacobi in Russia (Pavlova, 1968) and Spencer in England (Wyatt, 1851).

Jan 1, 2019

By G. van Aswegen

The geometry and morphology of a set of low-angle fractures around a stope in a deep Witwatersrand gold mine are explained in terms of extension fractures forming under variable conditions of stress. Primary extension fractures (E1) form some distance ahead of an advancing stope along the s1, s2 plane. With stope advance, a couple of these fractures end up in a stress regime conducive to transpressional shear and a secondary set of extension fractures(E2) is formed at a high angle to the primary fractures. i.e. at a low angle to the stope. As the E2 fractures are undermined, they migrate into a stress regime of transtensional shear and a third set of extension fractures (E3) may develop between E2 fractures. These have sigmoidal shapes, being parallel to the E2 fractures at the E2 discontinuity where s3 is negative, and curved through the unfractured rock between E2 fractures where s3 is positive at the instant of fracturing. The fractures all display fractographic features characteristic of dynamic extension failure with striae indicative of the direction of rupture propagation and the local, instantaneous orientation of s1.

Jan 1, 2012

By G. van Aswegen

The geometry and morphology of a set of low-angle fractures around a stope in a deep Witwatersrand gold mine are explained in terms of extension fractures forming under variable conditions of stress. Primary extension fractures (E1) form some distance ahead of an advancing stope along the s1, s2 plane. With stope advance, a couple of these fractures end up in a stress regime conducive to transpressional shear and a secondary set of extension fractures(E2) is formed at a high angle to the primary fractures. i.e. at a low angle to the stope. As the E2 fractures are undermined, they migrate into a stress regime of transtensional shear and a third set of extension fractures (E3) may develop between E2 fractures. These have sigmoidal shapes, being parallel to the E2 fractures at the E2 discontinuity where s3 is negative, and curved through the un-fractured rock between E2 fractures where s3 is positive at the instant of fracturing. The fractures all display fractographic features characteristic of dynamic extension failure with striae indicative of the direction of rupture propagation and the local, instantaneous orientation of s1.

Jan 1, 2012

By Juan Mendoza Mendoza Marsano

La primera actividad minera organizada en el Perú es el laboreo de oro de placeres, cuyo apogeo se ubicó en la provincia de Carabaya, Sandia(Puno) y Quispicanchis(Cusco) en el sur-oriente del país. En ese sentido, el presente trabajo describe los antecedentes históricos de dicha actividad durante la Colonia, la labor del banco minero, los logros del programa y el plan nacional de fomento a la minería.

Sep 1, 1974

By Jorge Olivari Ortega

EL presente texto describe el origen del oro en los imperioz inca y azteca, así como las zonas de sus producción. De acuerdo a las crónicas incaicas, el término "cori" significa oro y se creía qu el oro era lágrimas que el Inti había llorado. De otro lado, los "catucamayoc", eran los mercaderes que intercambiaban productos como el oro, plata y piedras preciosas en el mercado o "catu", cuyo funcionamiento coíncidía con las fiestas religiosas del lugar. En el imperio azteca, el término "Teocuitlatl" significa “oro” en náhuatl y es considerado como «excremento de los dioses». Este mineral se obtenía de uno de los productos de los pochtecas en los tianguis o ferias.

Jan 1, 2012

By Pedro Tumialán

Desde el siglo XIX el distrito minero de Hualgayoc ha sido objeto de estudio por el Banco minero y la Geological Survey de Estados Unidos, realizando explotaciones de minerales polimetálicos. Posteriormente se desarrollaron explotaciones de oro en los óxidos de los 16 mantos de del Compañía Minera Los Mantos, ubicada en Cajamarca. En este sentido, el presente texto describe el proceso de explotación de oro en el yacimiento de Hualcayoc, cuya mineralización de la plata y oro en los mantos, registra un bajo costo de operación a través del proceso de lixiviación realizado en las rumas. Asimismo, los mantos presentan una concentración residual del oro en los óxidos que duplica la ley original, disuelven parte de la plata, el cobre y el zinc y están ligados a exhalaciones volcánicas continentales en el Apitiano y marinas en el Albiano.

Aug 26, 1988

By Jorge Olivari Ortega

"El presente texto describe el origen etimológico de la palabra oro, propiedades e historia. El término oro deriva del latín aurum, cuya raíz refiere al color, gelb al color y ccori al origen. Este metal amarillo se encuentra en forma dendrítica, es decir, en masas arborescentes, masas redondeadas como pepitas «pepitas de oro» y en forma de escamas o pequeñas lámina. Entre sus propiedades tenemos: el color opaco, brillo metálico, maleable, dúctil sin ningún clivaje y de una fractura áspera y que prácticamente es inalterable e insoluble en los ácidos simples. El grado de concentración del oro en una mena (depósito que contiene mineral aurífero) es medido por la ley (cantidad de oro por tonelada de mena), mientras que su pureza es expresada en quilates. Los primeros indicios del trabajo con el oro en territorio peruano se remontan a unos 1500 años aC. Los primeros buscadores de oro prehispánicos obtenieron el metal amarillo de los placeres o depósitos aluviales, de los cuales se podían extraer fácilmente con la mano, las lentejuelas y las pepitas de oro."

Sep 1, 2015

By Korsch RJ

Permian oroclines in eastern Australia must have formed by sliding on a detachment surface. It is identified as a westward- dipping Devonian and Carboniferous sub- duction zone. Major strike-slip faults probably sole out on the same surface. One major fault with an associated serpentinite belt was pulled away from the craton abd bent into loops. Basins formed in the loops.

Jan 1, 1987

By R L. Brathwaite

The orogenic gold deposits wall poster is one in a series of posters on different mineral deposit types being produced by GNS Science to raise awareness of the characteristics of New Zealand mineral deposits and their prospectivity. Orogenic gold deposits are typically quartz vein deposits formed in fault and shear systems at crustal levels within and above the brittle ductile transition zone, at depths of 3 12 km and temperatures from 200¦ to 400¦C. In New Zealand, orogenic gold deposits are found in regionally metamorphosed sedimentary rocks of Paleozoic and Mesozoic age. The deposits in Paleozoic rocks include those at Golden Blocks in Northwest Nelson, Lyell and Reefton on the West Coast, and Preservation Inlet in Fiordland. Quartz veins are developed along shear zones that dip steeply and generally strike parallel to the axes of folding in the greywacke and argillite/slate host rocks, although most are discordant to bedding. The lodes are typically less than 1 m wide and extend an average 200 m horizontally and vertically, but the Birthday Reef at Blackwater, Reefton, the largest quartz vein deposit in Paleozoic rocks, averages 60 cm in width and was mined over a strike length of 1070 m, and to a depth of 830 m. Disseminated gold occurs adjacent to the quartz lodes at Globe-Progress and some other Reefton deposits. The deposits in Mesozoic rocks are hosted in schist of Otago and Marlborough, and schist and greywacke of the Southern Alps. The lodes are typically lensoidal, less than 1 m wide and localised along single or multiple parallel shear zones that generally dip steeply, and are discordant to the schist foliation and bedding. A notable exception is Macraes, where the lodes are developed in the semi-concordant, low angle Hyde Macraes Shear Zone that has a strike length greater than 25 km.

Jan 1, 2005

By R R. Large

"An EXTENDED ABSTRACT is available for download. A full-length paper was not prepared for this presentation. The formation of orogenic gold deposits is commonly a two-stage process. The first stage involves preconcentration of gold in a suitable source rock, such as carbonaceous black shales, felsic volcaniclastics or komatiitic volcanics. The second stage involves the release of gold (commonly with arsenic and/or tellurium) from the source rocks during metamorphism or magmatic intrusive events, accompanied by the replacement of source rock pyrite by pyrrhotite. Recent research suggests that synsedimentary gold trapped in the structure of diagenetic arsenian pyrite in reduced carbonaceous facies of continental margin sedimentary basins is an ideal source of gold for many orogenic and Carlin-style gold deposits. The conversion of diagenetic arsenian pyrite to pyrrhotite during basin closure and greenschist facies metamorphism is the key process releasing gold and arsenic to the metamorphic fluid, with metal deposition in structural trap sites to form the deposits.CITATION:Large, R R, 2015. Orogenic gold deposits – a two-stage process of gold enrichment, in Proceedings PACRIM 2015 Congress, pp 335–340 (The Australasian Institute of Mining and Metallurgy: Melbourne)."

Mar 18, 2015

By Ayokunle Adewale Akinlalu, Sunday Bayode, Sherif Olumide Sanusi, Joshua Oluwagbenga Adeboye

Gold occurrences have been reported in Alagbede, southwestern Nigeria, but a mineral potential map (MPM) to guide academics and investors in the area is still needed. As a result, geophysical methods (aeromagnetics and aero-radiometry) have been used to assess the potential for gold minerals in the area. Several enhancement filters, such as reduction to the equator, upward continuation, analytical signal, second vertical derivative, and power spectrum analysis, were applied to the aeromagnetic data to understand the subsurface geology better. The enhancement filters applied to airborne radiometry data are K/eTh, ternary color composite, F parameter, and deviation from the ideal K values (Kd). Geophysical data analysis was used for structural mapping and geological reconstruction, while aero-radiometric data was used for hydrothermal alteration mapping. The primary trend observed in the area’s magnetically inferred structural framework map is NE-SW, while a few are in the NW–SE and E-W trends. These observed trends show that the study area suffered at least three deformation episodes. Geological evidence of gold mineralization, such as favorable lithology, geological structure, and hydrothermal alterations, has been fused to produce a reliable MPM of the area. The geographical location of the existing mineral sites in the investigated area agrees with the geological structures and the MPM produced there. Thus, the systematic approach adopted in this study can be extended to other supracrustal belts of a typical Precambrian basement complex worldwide to ensure the reliability of orogenic gold mapping and resource management.

May 9, 2023

By J. Reinhardt, R. Uken, S. S. Chinnasamy

Au mineralization in the Kilpwal Gold Mine is confined to laminated quartz-carbonate lodes and associated alteration along the Klipwal Shear Zone (KSZ) in the upper Mozaan Group of the Mesoarchaean Pongola Supergroup. The brittle-ductile shear zone is characterized by inner and proximal hydrothermal alteration domains that are comprised of chlorite, epidote, sericite, pyrite, arsenopyrite and gold. Possible sources of gold are: (i) paleo-placer U-Au rich conglomerates from the lower Mozaan Group; (ii) the underlying mafic volcanics of the Nsuze Group; (iii) greenstone belts in the basement to the Pongola basin. Post-Pongola granites probably provided the heat to mobilize auriferous fluids into the KSZ.

Jan 1, 2011

By Andre Luis de Zorzi Marin

O corte a plasma de aço inoxidável tem história relativamente nova em comparação com outros meios de corte de metais. Frequentemente os usuários de corte plasma se deparam com questões específicas ao corte do aço inoxidável, como qualidade de corte, velocidade de corte, custo operacional e alterações nas propriedades metalúrgicas. Nos últimos vinte anos as tecnologias aplicadas no corte plasma do aço inoxidável tem evoluído com resultados atrativos nos últimos cinco anos. Estas tecnologias versam com alterações na mistura dos gases de plasma e de proteção, ou ainda, na mudança dos bicos de corte plasma buscando melhor constrição do arco plasma, e a devida seleção de gases em função da espessura de corte. Este trabalho foi desenvolvido através de revisão bibliográfica das principais tecnologias apresentadas pela indústria nas últimas duas décadas para o corte de aço inoxidável com plasma, e testes laboratoriais de corte com as últimas tecnologias de corte. Entre os resultados estão a redução até a eliminação da escória pós-corte, uma borda de corte menos arredondada, melhora na coloração da superfície e diminuição da zona afetada pelo calor na peça de trabalho. A importância do trabalho se dá pelo aumento da participação do uso do aço inoxidável dada a sua importância para a economia, em especial nos setores de energia, processamento de alimentos, papel e celulose e transportes que necessitam de melhorias no corte deste metal e suas ligas.

Jan 16, 2018

By Altair Lúcio de Souza

A laminação de tiras a quente com laminadores Steckel tem como característica um perfil de temperatura mais baixa nas pontas sendo este um dos motivos que geram cargas de laminação muito mais altas nesta região. A carga de laminação elevada tem como consequência no processo a geração de desvios de planicidade e o alto risco de rompimento do material nos passes finais de laminação. Este trabalho tem como objetivo demonstrar os benefícios da utilização da estratégia de Tapering para a laminação de tiras de espessura fina em laminador Steckel. Foi feita a comparação das cargas de laminação do material laminado e o acompanhamento dos resultados de planicidade obtidos antes e depois da implantação desta função. Ao fim do trabalho verificamos que a estratégia de Tapering é essencial para o processamento de materiais finos com laminadores Steckel.

Jul 30, 2018

By Ryosuke O. Suzuki

A new cell concept for calciothermic reduction is proposed in which the titanium dioxide instead of TiCl4 is used as the raw material for reduction, Metallic calcium is needed as the reductant of a thermochemicaily stable oxide, such as TiO2. CaCl2, is selected as the solvent of Ca and simultaneously as the solvent of CaO. The reduction system consists of a single cell where both the reduction reaction and the electrolytic reaction for recovery of reducing agent coexist in the same molten CaCl2 bath. A few mol%Ca dissolves in the melt and gives the media a strong reducing power. Sufficiently deoxidized metallic titanium deposits and forms a slightly sintered granular sponge. Both mechanisms of the halide flux deoxidation and the electrochemical deoxidation work efficiently for these fine precipitates, The reducing agent is in situ recovered by electrolysis of CaO because the molten CaCl2 he a relatively large solubility for CaO Some cell designs and modifications are proposed for industrial applications.

Jan 1, 2003

By AIME AIME

BORN a Chicagoan, on Aug;. 31, I879. Oscar Johnson lived in that city until young manhood. As a youth delivering newspapers he set his sight on the l university of Chicago and at sixteen years of age he began working summer vacations in the foundry of the Pullman Company. Misfortune came to his family during the summer of 1898 when tuberculosis took his only sister and brother. His mother, apprehensive of Oscar's health, urged him to try the West at least for awhile. So late summer found Oscar in Salt Lake City, employed by the Trent Engineering & Machinery Co. At that time it was busy building equipment for use in the war with Spain. Though he did not know it then, Oscar war was laying the groundwork for his present membership on the Mining Equipment Industry Advisory Committee of the W.P.B., a post which keeps him commuting between Denver and Washington.

Jan 1, 1944

By J. Priede, G. Gerbeth

"Two different instability mechanisms of electromagnetically levitated bodies are analyzed. The first is due to the virtual coupling between the electric current passing through the magnetic system and the variation of position of the body. This mechanism can result in unstable mass center oscillations of a levitated solid body. Another type of instabilities may occur because of the coupling between the motion and the electric currents induced in the body. This effect can cause a spontaneous rotation of the body setting in as the frequency of the alternating magnetic field exceeds certain critical threshold depending on the configuration of the field. This instability can be suppressed by an axial steady magnetic field of strength comparable to that of the levitating field. 1 IntroductionAn alternating magnetic field interacting with eddy currents induced in a conducting body causes repulsion between the body and the coil generating the field. Besides, the eddy currents provide a contactless heating of the body. In such a way metallic samples can be levitated and melted without a contacting crucible. This technique allows to avoid contamination of the melt with container material and so to achieve a considerable super-cooling of the melt before it solidifies. Nowadays electromagnetic levitation is widely used in material research for measuring of the thermophysical properties of molten metals (2) .It has been observed since early fifties when the first experiments on the electromagnetic levitation were done that under certain circumstances solid levitated samples start to rotate or oscillate [l]. Surface oscillations can appear in addition when the sample is melted. Such phenomena are undesirable because they often result in failure of the levitation. Recently we showed that rotational as well as oscillatory instabilities can have electrodynamic origin related to additional eddy currents induced by motion of the body in an alternating magnetic field [3] , [4].In the first part of the present paper we analyze another possible cause of oscillatory instability due to the coupling between the electric current passing trough the magnetic system with variation of the position of the levitated body. The second part of the paper deals with the origin and suppression of rotational instability in a uniform alternating magnetic field."

Jan 1, 1999

By T. G. Joseph

"The Oil sands-Equipment Interactions Program (OsEIP) is a collaborative research venture between Syncrude Canada Ltd., James Progithin International Ltd. (JPi), the University of Alberta, P&H MinePro, and Caterpillar Inc. The objective is to better understand the behaviour of oil sands as it interacts with mining equipment, in particular, large trucks and shovels. With a move to ever larger equipment, mining oil sands of highly variable bitumen content, ground stability comes into question. This paper outlines this aspect of OsEIP and provides some insight into how some of the findings enable an improved understanding of oil sands behaviour that may impact large equipment design, operational and maintenance strategies. IntroductionThe mechanical behaviour of oil sands in the underfoot and in the face yields some of the harshest stability and digging conditions of any mining environment. High maintenance costs from truck and shovel fatigue failures predominate as a result of ground stability issues. Wear rates of shovel and dozer ground engaging tools (GET), rollers, roller paths and crusher screens result in costly and frequent replacement, or even more frequent and costly sacrificial wear zone building. From the shovel face to the crushers and screens, dry oil sands mechanics affects the degree of fragmentation and, ultimately, bitumen production.An increased knowledge of the behaviour of oil sands with respect to stability, fragmentation and abrasion, etc. would enhance the long-term equipment design process at the vendor level, and provide the end user with improved short-term operational guidelines and long-term strategies for future purchases and operation. Truck vendors recognize that the interaction between operator, seat, frame, suspension, tires and oil sands is unclear, and must be better understood before proceeding to next generation designs. Similarly for shovel manufacturers, the relationship between bucket/dipper motion, carbody, side frame, rollers, track and oil sands follow in the same vein."

Jan 1, 2002