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By Jorge Alberto Soares Tenório, Denise Crocce Romano Espinosa, Beatriz Peralta Oruê

Manganese, a toxic mineral, related to manganism may have high added value for the steel industry. The difficulty in obtaining manganese encourages the exploration of new secondary sources such as the lateritic nickel effluent. In Brazil, nickel reserves are predominantly lateritic, making the country a potential producer. For the tests, a synthetic solution was used which simulates the lateritic nickel effluent from leaching. The oxidative precipitation with ozone occurred at the oxygen flow rates: 0.5; 1.0 and 2.5L/min, at the original pH 1.5 at 21°C in a 500 mL bubble column reactor. O3 was produced in the benchtop generator feed by 99% oxygen. The ozonation time was determined by the oxidation potential1.55V. The ozonated solution was centrifuged and filtered. The filtrate and collected samples were characterized in ICP-OES. Optimization tests with ultracentrifuge were performed. The best precipitation reached 97% at 0.5L/min O2 at 6.07 ± 0.045mg/min of O3 dosage and resulted in a solution 10-15mg/L Mn+2, above 1mg/L, maximum value acceptable by Conama 2011, to be retreated before being discharged into the water body or being reused as a manganese source.

Oct 3, 2019

By Gustavo Menezes Nevesr

Este trabalho tem como objetivo apresentar os resultados do procedimento de adequação do sistema de geração de vapor na CTE-1, visando à redução de custo no grupo CSN. O estudo foi efetuado através da avaliação das condições operacionais dos equipamentos e análise dos processos de geração de energéticos da planta CTE-1, aos quais permitiram diagnosticar as melhores práticas e definir a melhor configuração. Os resultados apresentados foram significativos para as condições de operação atual, o que representa redução do custo para o grupo CSN. Com redução do consumo de vapor e energia.

Sep 25, 2017

By Dimas Pereira Coura, José Geraldo da Silva Moreira, Eder Quental de Araújo

O território brasileiro devido a sua localização na região tropical, possui um grande potencial para aproveitamento de energia solar. O objetivo deste trabalho é dimensionar um sistema que aproveite a energia solar por tecnologia fotovoltaica no setor siderúrgico, o qual é um dos maiores consumidores de energia elétrica da indústria. O estudo é voltado as usinas siderúrgicas integradas a coque, e se baseia no aproveitamento de área instalada em telhados de galpões, para o qual foi definido uma área padrão para facilitar a análise, definição de ângulo de inclinação dos painéis, quantidade utilizada, análise de interferências e posteriormente realizado viabilidade do sistema considerando as diferentes taxas de irradiação de acordo com a localização geográfica de cada usina.

Aug 1, 2019

By R. J. P. Lyon, A. E. Prelat, H. Lawrence

Introduction In 1977, the US Bureau of Mines awarded a grant to the state of South Carolina to explore the possibility of using Landsat multispectral scanner (MSS) data as an aid in monitoring surface mining activities in selected counties of the state. Work had been done in Aiken County prior to the grant by USBM and state personnel at the EROS Data Center using both the GE Image 100 and ESL IDIMS systems. The initial work on the 1:100 consisted of locating and measuring the areas of various kaolin mines. The results were excellent on location, identification, and accurate area measurements of several mines as compared with aerial photos of each mine. The effort also included locating and measuring the size of all mines (including sand and gravel) within two US Geological Survey (USGS) 7 % - min quadrangle maps. Line printer overlays using the IDIMS equipment and software resulted in the location of all known mines within an estimated error less than zt 91.4 m. Mine acreage was calculated by counting each symbol (which represented one pixel) and multiplying by 1.1 (the number of acres per pixel). [Fig. 1] shows a portion of one quadrangle overlay. [Table 1] gives a comparison of acreage measured for several mines from the 1-100 and IDIMS system vs. aerial photo measurements. The success of the preliminary work resulted in the South Carolina Land Resources Conservation Commission submitting a proposal to USBM for funding to expand the scope of work to other mineral mining operations within the state and determine if Landsat Imagery could be used to accurately locate and measure mining and reclamation activity on a continuing basis. Three separate tasks were proposed for selected kaolin mines in Aiken County: Task 1, to measure changes in active mine developments over the period 1974-77; Task 2, to measure reclamation activity, and, if time permitted, seasonal changes in mine signatures over the same period of time; and Task 3, to classify one complete mining operation (i.e., differentiate between active, spoil, overburden, water, reclaimed portions and surrounding terrain. The major effort was centered around J.M. Hubeis Richardson mine. Mining operations were progressing in a northerly direction and included three areas of reclamation: one prior to 1974; one started during early 1974; and one reclaimed during 1976. A discussion of all work done under the grant is available in the March 1979 Final Report listed under References. Computer compatible tapes (CCTs) containing MSS data from Landsat Path 18, Row 37, were purchased from the National Aeronautics and Space Administration (NASA) covering the period February 1974 through January 1977. The MSS data were processed on the General Electric Image 100 using parallelepiped classification at the EROS Data Center's Data Analysis Laboratory, Sioux Falls, SD, and at the Stanford Remote Sensing Laboratory, Stanford University, Palo Alto, CA, utilizing both an unsupervised classification (ISOMIX) and a supervised classification (sequential discriminant analysis). Studies at Stanford University Remote Sensing Lab (SRSL). In Feburary 1977, initial work was begun at Stanford using the STANSORT computer program running on a DEC PDP-10 (Honey, Prelat, and Lyon, 1974). This software is fully interactive and designed to study Landsat CCT data at high resolution (small areas) on a pixel-by-pixel basis (Lyon, 1977). Unsupervised Classification. The initial step was to locate the Richardson mine on the positive print of the full Landsat scene from CCT 1644-15252, dated 6/17/74. This was relatively easy due to a large abandoned kaolin mine and a long narrow pond clearly visible in the scene. Two unsupervised classifications of the Richardson mine were run using ISOMIX clustering (Honey, Prelat and Lyon, 1974). (ISOMIX essentially follows the interactive clustering procedures of ISOCLS Kan, Holley, and Parker. 1973). Although the classifications were successfully accomplished, it was apparent from the TV display that the results did not clearly define the mine areas. A supervised classification would have to be made in order to clearly separate each portion of the mine. Supervised Classification. This classification was done using the Stepwise Discriminant Program (BMDO7M) which is part of the BIOMED package (Dixon, 1970) and involved the following steps: Training group populations were selected and the digital

Jan 1, 1982

By Eder Quental de Araújo

É apresentado o Balanço Energético Global da Gerdau Ouro Branco 2016, com os principais indicadores de consumo energético das áreas produtoras. Além dos indicadores energéticos globais, o balanço apresenta os consumos físicos específicos de cada insumo nas diversas áreas, permitindo a análise de cada setor da usina isoladamente. Destaca-se em 2016: - Início de operação do Laminador de Chapas Grossas. - Maior produção de laminados da história da Usina Ouro Branco.

Jan 26, 2018

By Luiz Fernando Pimentel Simões

Neste trabalho são apresentados o planejamento e preparação para o início da operação, o período de “ramp up” e estabilização da produção da sinterização da Companhia Siderúrgica do Pecém. Incluindo a estruturação e execução do comissionamento; elaboração dos procedimentos para operação aliado a implantação do sistema de gestão da qualidade; definição do quadro de pessoal, seleção, contratação e treinamento; definição das especificações de matérias-primas, aquisição dos primeiros lotes, com desenvolvimento de fornecedores locais; apresentação dos resultados dos principais indicadores de produção e qualidade no período de “ramp up” e estabilização da planta.

Oct 30, 2017

By L. C. IlsLey

Minin,g Qr col-cu.ttint till:I chines are 1?;\i9ng the _m9t wideiy .used de1sses ()f mining equipment.· These 1T:.i:1Chines ,.--re practicaily t-tl\·operc1_ted eiyher_by compressed .iir or by electric. ·motors. According to &.ta• compiled _ from the 122. issue COAL CATALOG\JE. OJMEINED WITH; OOAL "FIELD 'pf!:fC'TOTl1, bf 7,088. mnes from which reports were obttiined there -are 3895 mines that u.se coal-cutting eql;lipmen:ts,, 'f'hi report lists 20,031: r.ct:lchines, 17,&75 being operated by·elct:i.c.m<;>_tors··:r;id :the remtiinder by compressed i.r motors,· ,-. · ', .. . · .. ··, .. _ ,· .,, .. .. . . . . . : ; "'l t:: On tl.Ccou-nt .. of the wide· use of coc:11-cutting -.:i"cliine_- any Stat!;ls have issued regulationa as "to their operation dnd be to safety precautions that.should be observed J especially in gaseous mines.

Oct 1, 1922

By Thompson Júnior Ávila Reis

Neste trabalho, a microscopia de força atômica foi empregada para estudo da evolução da fragilização a 475ºC em um aço inoxidável lean duplex. Para tal, amostras deste aço foram submetidas a tratamentos isotérmicos com duração variando entre 1 e 100 horas na temperatura de 475ºC. Ensaios de tenacidade ao impacto e de dureza foram realizados para confirmar a ocorrência da decomposição da fase a. Posteriormente foram realizadas análises no microscópio de força atômica. Os ensaios de tenacidade ao impacto e de dureza indicaram que ocorreu decomposição espinodal da fase a. Medições da diferença da dissolução das fases a e ?, conduzidas no microscópio de força atômica, indicaram que a resistência à dissolução da fase a diminui com o tempo de envelhecimento de forma similar a redução da tenacidade. Os resultados indicam que a microscopia de força atômica é uma ferramenta eficiente para avaliar o grau de evolução da fragilização a 475ºC.

Aug 16, 2017

ALABAMA. Aldrich.-Aldrich, W. F. Anniston.-Noble, A. E., 20th St. and Wilmer Ave. Auburn.-Brown, R. L., Box 0. Bessemer.-Abbott, C. E., T. C., I. & R.R. Co. Ferguson, V., U. S. C. I. Pipe & Fdy. Co. Williams, E. P., Tenn. C., I. & R. R. Co. Birmingham.-Aldricb, T. H. Aldrich, T. H., Jr., 406 Woodward Bldg. Allen, A. W., 1616 S. 14th Ave. Bowron, J., 1401 S, 20th St. Burbidge, T. A., Browu-Marx Bldg. Coxe, E. H., Tenn. C., I. & R. R. Co. Crawford, G. G., Tenn. C., 1. & R. R. Co. Crockard, F. H., Woodward Bldg. Dimmick, F. D., Dimmick Pipe Co. Ellis, E. E., 1515 Brown-Marx Bldg. Fairbairn, C. T., Woodward Bldg. Fies, M. H., 2316 Highland Ave. Hiller, E., 516 Brown-Marx Bldg. Hillman, M. P. G., 707 Empire Bldg. Ludwig, C. P., 12th Ave. and 12th St. McCormack, G. B., Lookout Mt. Iron Co. McCrery, C., Tenn. C., I. & R. R. Co. Moffett, C. A , 909 Brown-Marx Bldg. Peters, R.. Jr., Brown-Marx Bldg.

Jan 1, 1917

By Daniela Oliveira Mota Guimarães

As inclusões de sulfeto de ferro são indesejáveis no aço, pois são responsáveis por causar o fenômeno de fragilização a quente. A relação entre manganês e enxofre se torna de plena importância para o entendimento desse fenômeno. O presente trabalho teve como objetivo indicar a relação entre Manganês (Mn) e Enxofre(S) mais adequada para a não ocorrência deste fenômeno, e explicar a influência dessa relação nas propriedades dos aços C-Mn. Estudou-se um aço C-Mn com a relação Mn/S 50% menor do que a relação visada na Companhia Siderúrgica Nacional(CSN).

Aug 16, 2017

By Adriano Francisco dos Santos

Dentre as diversas atividades executadas na área de Utilidades de uma empresa, o processo de clarificação e potabilização da água é de suma importância para a manutenção dos processos e das pessoas que ali trabalham. O presente trabalho visa mostrar a preocupação da Área de Energia com os funcionários, colaboradores e comunidade, no que se diz respeito aos riscos a saúde e segurança na utilização do cloro gasoso no processo de clarificação e potabilização da água e as atitudes tomadas para eliminação desse risco, durante o processo de substituição do cloro gasoso pela tecnologia Oxamine®.

Jul 31, 2018

By Eduardo Candido de Almeida Wenceslau

O laminador reversível 4-HI de uma cadeira da CSN-PR, o LRF#1 tem capacidade de projeto de 350kton/ano, suficiente para atender a linha de galvanização contínua, LGC, que produz o Galvalume?, primeira unidade no país até sua partida. Deficiências na produtividade desse laminador passaram a ser fator de atenção, pois acarretava na necessidade de complementação de abastecimento de bobinas full hard, BFH, provenientes de outros laminadores do grupo. O presente trabalho mostra o estudo e plano de ação realizado para incremento da produtividade do laminador, sobretudo por meio da redução do número de passes de laminação e revamp do sistema de refrigeração para atender plenamente a demanda da LGC com baixo custo e possibilitar o fornecimento de BFH a clientes externos.

Jul 30, 2018

By W. A. Tiller, J. D. Harrison

HOT pressing of powder particles has gained importance recently, since it affords a method in which high densities are rapidly attained. In a recent study on hot pressing of alumina powders, Mangsen, Lam-bertson, and Best1 have shown within the limits of their experiment, the validity the rate equation for densification in hot pressing, originally proposed by Murray, Livey, and Williams.2 i.e., where D = fraction of theoretical density, t = time, P = pressure and 77 is the viscosity, all in appropriate units. This equation was derived from earlier work of Shuttleworth and Mackenzie3 which is based on the closing of spherical pores under the action of surface tension. The integrated form of this equation yields a straight-line relation between log (1 - D) and t. Such conditions were found by Felten4 to be true only after extended periods of pressing. In an endeavor to quantitatively evaluate the exactitude of this equation in the initial sintering stage, i.e., prior to sealing of the pores, spherical anti-

Jan 1, 1962

By J. Shibata, N. Murayama, H. Yamamoto

As one of effective usages of wastes discharged in the non-ferrous metal industry, the syntheses of AlPO4-5 and hydrotalcite were carried out using aluminium dross as a raw material. AlPO4-5 is an aluminium phosphate condensate with properties of zeolitic materials and large pore size. Hydrotalcite is an inorganic anion exchanger and has a layered structure of complex hydroxide. They were synthesized in an autoclave at high temperature and pressure. Various physical properties such as crystal structure, surface texture, and specific surface area were measured. AlPO4-5 can be synthesized from aluminium dross under hydrothermal conditions at 180°C-200°C, and 3h. At the same time, AlPO4-34 and non-porous AlPO4 were also formed as by-products. The crystals of AlPO4-5 have a hexagonal structure. Lt is desirable to heat the reaction product at around 550 °C to remove tri-ethyl amine. The specific surface areas of the reaction product before and after heat treatment at 550°C were 17.9m2/g and 358m2/g, respectively. Hydrotalcite can be obtained by a co-precipitation method from the aluminium dross and waste MgCl2 solution discharged in the aluminium regeneration process. Small amounts of SiO2, Al2O3, and Fe2O3 remain in the reaction product as an impurity component. The interlayer distance of the obtained reaction product is about 0.3 nm. Hydrotalcite changes to Mg-Al oxide during calcination at 500 °C for 3h, and then hydrotalcite is formed again by a rehydration operation. The physical properties of the reaction products obtained from the wastes were very similar to those from fresh reagents.

Jan 1, 2004

By Flanelson Maciel Monteiro

Os materiais cerâmicos são essenciais para o desenvolvimento da humanidade. O homem os utiliza para os mais variados fins, desde a confecção de utensílios domésticos até a produção de peças de alto desempenho tecnológico. Neste sentido, são extremamente necessárias à produção de pesquisas científicas para prospectar novos materiais para a indústria cerâmica. As argilas são consideradas o principal componente para fabricação de massas cerâmicas. Para produção de peças de cerâmica branca, revestimentos e outras categorias cerâmicas onde a coloração clara é prioridade, usam-se argilas cauliníticas. Todavia, esse tipo de argila possui pouca ocorrência na esfera terrestre, em comparação com outros tipos, tais como as argilas de coloração vermelha. Por tal motivo, encontrar novas jazidas de argila caulinítica para abastecer à indústria ceramista é extremamente imprescindível. Nesse sentido, objetiva-se com esse trabalho caracterizar uma argila caulinítica proveniente de uma jazida localizada no município de São Gonçalo do Amarante, região metropolitana de Natal-RN. O referido trabalho configura-se como a primeira parte de uma caracterização do material estudado. Sendo reservado para esse artigo os ensaios físicoquímicos e na segunda parte os ensaios tecnológicos. A caracterização fisioquímica foi realizada através das seguintes análises: DRX, FRX, Análise Granulométrica (AG), Dilatometria e ATG/DTG. Os resultados obtidos demostram a viabilidade técnica da utilização do material para fabricação de produtos cerâmicos, tais como: telhas, lajotas, revestimentos e outros materiais cerâmicos.

Oct 30, 2017

By Marc C. Bétournay

Hydrogen fuelcells are a known technology, having been applied to stationary (e.g equipment, buildings, power plants) and vehicle applications (e.g transit buses, space shuttles). There is currently a growing need to provide alternate power systems to diesel fuel for underground mining vehicles to improve underground air quality and reduce production costs and green house gas emissions. To date, however, fuelcells have not been exposed to underground mine air and physical conditions. A testing program was carried out to provide information on the vulnerabilities of fuelcells as part of a number of proof-of-concept projects to apply hydrogen power to underground mining vehicles. The fuelcell type of choice for the industry, the Proton Exchange Membrane, would function at the range of temperatures encountered in underground and surface operations, and use hydrogen that is stored under low pressure and risk. A small fuelcell stack was tested in a cooperative project between CANMET, the Fuelcell Propulsion Institute, INCO, the Ontario Ministry of Labour, Sandia National laboratories and H-Power. This article will review the tests carried out to measure the effects from high humidity, mineral dust, diesel emission gasses and diesel particulate matter as well as from shock and vibration provided to the unit in underground conditions, at INCO?s 175 Orebody minesite and INCO?s Stobie Mine. The test results provided will show that the unit was not affected by the underground conditions: physically and electrically the unit performed without any reduction in operation or adverse effects imposed.

May 1, 2003

By Antônio César de Araújo Freitas

As empresas de mineração têm desafios logísticos em sua operação no dia a dia, visto o crescente volume de minério movimentado nas Usinas e Portos e pressão crescente por resultados operacionais que se traduzem na busca contínua por níveis superiores de produtividade. A tecnologia de automação dos processos produtivos e de máquinas evoluiu muito na última década, entretanto o processo da logística nos pátios de matéria prima e produtos apresenta baixo nível de automação e é baseado em informações verbais e observações visuais a respeito do nível de estoques e disposição dos materiais nas pilhas e áreas dos pátios de manuseio. Em um processo tão complexo, pequenas decisões da operação no dia a dia, que podem variar de acordo com o operador, supervisor ou turno de operação, podem influenciar a produtividade diretamente, afetando indicadores como horas paradas e deslocamento de máquinas por tonelada expedida, afetando dessa forma custos significativos na operação de uma usina ou porto. Este trabalho tem por objetivo então descrever as técnicas utilizadas para modelar os desafios de logística nos pátios de minério, descrevendo sistemas de otimização utilizados com apresentação de resultados em projetos como o de Carajás, planta da VALE que é atualmente a maior mina de minério de ferro do mundo, abordando a redução de deslocamento de máquinas, diminuição da exposição ao risco de colisão e redução de paradas.

Jul 30, 2018

By Alexandre Rodizio Bento

A competitividade do setor automotivo exige maior agilidade na gestão de ferramentas de usinagem. Para atender esta necessidade flexibilizar e automatizar o processo de gestão de armazenagem é fator primordial. As ferramentas de usinagem muitas vezes têm custo elevado e a necessidade de controle constante é imprescindível no setor automotivo. A padronização de armazenagem aliada a um equipamento específico para controlar ferramentas surge como uma opção. Pois, a troca de produtos deve ser ágil durante a fabricação para evitar perdas e máquinas ociosas no chão de fábrica. Assim, suprir esta necessidade com velocidade é essencial e de suma importância para a integração entre os departamentos de produção e logística. Neste cenário, a tecnologia de armazenagem permite agilizar e flexibilizar a gestão de ferramentas de usinagem, além de possibilitar ganhos de produção. Neste trabalho, apresenta-se a substituição do processo manual de armazenagem de ferramentas de usinagem baseado em caixas e prateleiras, por um sistema com tecnologia de armazenagem vertical. Esta substituição permite automatizar o controle de ferramentas, reduzir o custo de estoque e flexibilizar a troca de produtos na produção. Os resultados deste processo permitem garantir a melhor gestão das ferramentas de usinagem, evitar paradas nas linhas, reduzir custos operacionais e manter estoques em perfeito equilíbrio, entre o aumento de produtividade e a redução de custos.

Aug 8, 2018

By Bradley S. Van Gosen, Anjana K. Shah, George M. Bedinger, Donald I. Bleiwas, Karl J. Ellefsen

"Ancient and modern coastal deposits of heavy mineral sands (HMS) are the principal source of several heavy industrial minerals, with mining and processing operations on every continent except Antarctica. For example, HMS deposits are the main source of titanium feedstock for the titanium dioxide (TiO2) pigments industry, obtained from the minerals ilmenite (Fe2+TiO3), rutile (TiO2) and leucoxene (an alteration product of ilmenite). HMS deposits are also the principal source of zircon (ZrSiO4), from which zirconium dioxide (ZrO2) is obtained for uses mostly in refractory products. Sometimes monazite [(Ce,La,Nd,Th) PO4] is recovered as a byproduct mineral, sought for its rare earth elements, and thorium (Ault and others, 2016; Sengupta and Van Gosen, 2016; Van Gosen and Tulsidas, 2016).HMS are sediments containing dense (heavy) minerals that accumulate with sand, silt and clay in coastal environments, locally forming economic concentrations of the heavy minerals (Fig. 1). Economic (mined) HMS deposits include Holocene sediments on modern coasts, such as examples in India and Brazil, as well as coastal deposits formed by transgressions and regressions of the seas during intervals in the Quaternary, Tertiary and Cretaceous, such as in Australia and the southeastern United States. Economic deposits typically contain heavy-mineral concentrations of at least two percent. Individual heavy minerals are commonly defined as minerals with a specific gravity greater than approximately 2.9 g/cm3. These minerals are generally resistant to chemical weathering and physical degradation and thus survive well in fluvial and coastal environments. Heavy minerals in coastal HMS deposits may include, in order of general abundance, ilmenite, leucoxene, rutile, magnetite, zircon, staurolite, kyanite, sillimanite, tourmaline, garnet, epidote, hornblende, spinel, iron oxides, sulfides, anatase, monazite, cassiterite and xenotime. Of these, ilmenite, leucoxene, rutile and zircon are the primary economic minerals. Garnet, monazite, cassiterite and xenotime are occasionally recovered as byproducts. The heavy minerals as a suite typically make up no more than 15 weight percent of a deposit and usually much less. Quartz and clay minerals form the bulk of the sediment. The geology of HMS deposits and examples of significant districts are summarized in Van Gosen and others (2014) and Hou and Keeling (2016)."

Oct 1, 2016

By E. C. Robertson

D.G. Wilder I found the suggestion that the amount of displacement of a fault can be numerically related to the thickness of gouge or breccia to be both intuitively satisfying and intriguing. I have long agreed that there is some type of relationship between the amount of gouge and the amount of displacement of faults. I congratulate the author for developing a numerical relationship between them. However, I am concerned that the limits for applying this relationship be fully understood. An underlying assumption in this approach is that there is either a uniform thickness of gouge or breccia along a given fault or the thickness does not vary widely. Since it is not always possible to confirm this, the displacements derived by this method should be viewed with caution unless significant fault extent can be observed. At the Nevada Test Site, in drifts constructed in granite for test emplacement of spent nuclear reactor fuel, we found a fault with 0.3 to 0.4 m (12 to 16 in.) of clay gouge. Within a few meters of this location, the fault had no clay gouge, but rather consisted of a highly fractured zone with significantly altered rock and some slickensides. Based on Fig. 1, the 0.3 to 0.4 m (12 to 16 in.) thickness of gouge would indicate a displacement in excess of 30 m (98 ft). However, no gouge thickness would indicate essentially no displacement. Based on a quartz vein that terminated on the fault, and is not identified nearby, an estimated displacement of more than a few meters was made. This estimate is consistent with that obtained using the regression line proposed in the paper if the 0.3 to 0.4 m (12 to 16 in.) thickness for the gouge is used. However, using the regression curves with zero thickness would not yield results consistent with what was observed in the field. Therefore, it is important to recognize that the suggested procedure would properly yield a range of probable displacements. ? *Work performed under the auspices of the US Department of Energy by the Lawrence Livermore National Laboratory under Contract W-7405-Eng-48. Reply by E.C. Robertson It is certainly true that the t (thickness) of gg-bx (gouge and breccia) on a fault does vary along the fault. My observations have been that near the termination of a fault, the displacement d is small and the t is also small, whereas the maximum d and t will usually be found in the central part of the fault. The information on gg-bx and t of the fault found in granite in the NTS tunnel by Mr. Wilder could be interpreted somewhat differently than he does. He speaks of the fault changing within a few meters from 0.3 to 0.4 m (12 to 16 in.) of clay gg to "a highly fractured zone with significantly altered rock and some slickensides," but no gg. The highly fractured rock may be taken to be bx, rock not so finely ground as gg but still crushed by the fault movement, equivalent to the gg in my usage, and probably occupying about the same t. Mr. Wilder&apos;s estimates for the fault in the NTS tunnel for t of 0.3 to 0.4 m (12 to 16 in.) and for d of a quartz vein, in excess of "a few meters," would place the point on the low side of the central trend line in my Fig. 1, at the lower limit. There is, of course, a problem with determining d using displacement of only one planar surface. It would be greater or lesser depending on the rake of the movement. Finally, estimating the d of a fault from its t should be made with awareness of our present uncertainties, as pointed out by Mr. Wilder. Although the central trend line in my Fig. 1 has a ratio of d/t of 100, I have put the limiting ratios at 10 and 1000. Understanding of the values of the ratio will be improved only with collection of more data, for which the discussion of Mr. Wilder is much appreciated. G.C. Waterman E.C. Robertson&apos;s paper provides significant information to a geologist attempting to deduce fault offset by noting the products of structural dislocation. However, considerable mapping in underground and open-pit mines, and examination of structures produced in different geological settings, have convinced me that gouge and breccia thickness are controlled by geological conditions and fault movement. The following paragraphs suggest geological variables that control them. 1. Depth of Loading A near-surface fault resulting from tensional stress has more breccia/gouge than is produced by a similar stress at considerable depth. A deep-loaded compressional stress may produce a linear zone of schist, or structural dislocation may occur along an earlier formed belt of schist. Such "shear zones" are common in Canadian mines in precambrian rocks. In neither case can offset be directly deduced by an analysis of the minimal gouge/breccia in the shistose rocks. At greater depth, stress may be partially to wholly relieved by flowage. I vividly recall first noting the regional "Midas Thrust" in the Lark mine, Bingham Mining District, UT (where we called the structure the North Fault). My recorded notes, as I remember them, showed a narrow gouge streak separated the `Jordan" and "Commercial" limestone units from impure, muddy limestone beds of uncertain stratigraphic position. The visible structure did not indicate the great importance of this premineral fault

Jan 12, 1984