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Micro-Pile Foundations in Difficult Subsurface ConditionsBy D. Dreher Whetstone, Paul M. Blakita, Christopher M. Reith, Ravi P. Malviya
"Micro-piles are small diameter (5 to 10 inches), cast-in-place piles which can develop high load capacities by bonding with soil or rock. Micro-piles are particularly well-suited for moderate to heav
Jan 1, 2005
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The Computational Modelling of Conveyor Belt Fires in Mine GalleriesBy D Giddings, S A. Silvester, S Pickerin
Underground fires represent a constant threat to the safety of underground personnel. Miners in the immediate vicinity may face intense heat, blinding smoke, toxic fumes, fall of ground and other dire
Jan 1, 2005
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Automated Textural Classification of Iron Ores Using æRecognitionÆ ù A Specialised Software Package for Studying Iron OresBy J M. F Clout
Geological, textural and mineralogical classification of iron ores is routinely conducted by mine and exploration geologists on reverse circulation percussion, blasthole cone and bulk samples for grad
Jan 1, 2005
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3D Characterization And Analysis Of Particle Shape Using X-Ray Microtomography (XMT)By J. D. Miller, C. L. Lin
In the processing industries, it is well known that particle shape is an important factor which determines the behavior of particulate systems. For example, system properties of technological signific
Jan 1, 2005
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Implications of Using NATM in Underground ConstructionBy Mohammad Irshad, Klaus Mussger, Harald Wagner
Despite the fact that the New Austrian Tunneling Method; NATM, has been used in the United States for the past 23 years or so, still considerable misconceptions exist in the industry about the nature
Jan 1, 2005
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Interactions Between Magnetite Oxidation, Calcination of Carbonate Minerals and Melt Formation in Iron Ore PelletsDuring induration of iron ore pellets produced from magnetite concentrates, there are many reactions occurring simultaneously. While the magnetite is being oxidised to hematite, carbonate fluxes are b
Jan 1, 2005
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Sustainable innovation in underground hardrock mining technologyBy A. Bamber
Canadian leadership in a global mining context will depend not only on entrepreneurship and best practice but also on technological innovation. This paper argues for more ambition and commitment to R&
Jan 1, 2005
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Industrial Minerals 2004 - ZeolitesBy T. H. Eyde
Estimated natural zeolite production worldwide during 2004 remained at about 3.6 Mt (4 million st), about the same as in 2003. China continues to be the largest producer of natural zeolites followed
Jan 1, 2005
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Shaft Hoisting Based on Direct Torque Control TechnologyBy Y Wu, F-J Ping
Today, coal production accounts for about 65 per cent of the nationÆs gross energy in China. By the year 2010, the output of coal is planned to increase to 1.65 billion tonnes and by the year 2020 to
Jan 1, 2005
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Role Of Magmatic Fluids In The Formation Of Seafloor Hydrothermal DepositsBy Steven D. Scott
The source of ore metals for base and precious metal volcanogenic massive sulfide (vms) deposits has been debated for decades. Metals can be obtained from high-temperature sea water-rock reactions in
Jan 1, 2005
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Advancing Comminution And Flotation Performance With Advanced Process ControlOften plant performance suffers as a result of poor control. Poor control leads to low mill throughputs, poor classification and less than satisfactory concentrate grades and overall recoveries. By
Jan 1, 2005
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The Contribution of the on-line Coal Analysers to the Sustainability of Greek Lignite Mining SectorBy M. Galetakis, C. Roumpos
A sustainable coal industry needs to achieve a number objectives concerning mainly with superior utilisation of deposits and improved environmental performance. Modern quality control systems, which a
Jan 1, 2005
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Electrical Resistivity Tomography In Urban Areas: A Case Study In Hania, GreeceBy I. Papadopoulos
Nowadays, geophysical prospecting is implemented in order to resolve a diversity of geological, hydrogeological and geotechnical problems. Though plenty of applications and a lot of research have been
Jan 1, 2005
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The Evolution of Materials for Pipeline ApplicationsBy D. Embury
The construction and utilization of oil and gas pipelines is a vital aspect of the Canadian economy. The evolution of materials for this application can be considered as part of an evolutionary proces
Jan 1, 2005
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Spontaneous Combustion and Simulation of Mine Fires and Their Effects on Mine Ventilation SystemsBy H W. Wu, D Humphreys
The structure of a comprehensive research project into mine fires study applying the Ventgraph mine fire simulation software, preplanning of escape scenarios and general interaction with rescue respon
Jan 1, 2005
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Volcanogenic Massive Sulfide Deposits in New ZealandBy R L. Brathwaite
In New Zealand, volcanogenic massive sulfide (VMS) deposits are found in three main geological environments associated with: 1. ophiolitic basalts of Oligocene age in Northland and East Ca
Jan 1, 2005
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Research Needs in Regard to Design, Performance Criteria, Construction, Maintenance Assessment and Repair of Coal Mine SealsLegislation introduced for Queensland and New South Wales Coal mines provides different levels of prescription regarding specification of mine seals û generally in relation to capacity to withstand ov
Jan 1, 2005
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Numerical Modelling of Undermined River Valleys ù A Case StudyBy J W. Lee, E Baafi, N Aziz
Ground subsidence due to mining is a common dilemma confronting the underground coal mining industry. The effects of underground longwall mining on river valleys have come under scrutiny, especially w
Jan 1, 2005
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Separation of Pyrite and Arsenopyrite in a Gold Sulfide ConcentrateBy D E. G Connelly, K Y. Wong
Gold at the Harbour Lights Mine (HLM), WA occurs principally in pyrite (Py) and arsenopyrite (AsPy) minerals rendering it inaccessible to direct cyanidation. Froth flotation produces a concentrate wit
Jan 1, 2005
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Mineralisation and Structural Setting of the Rise and Shine Shear Zone, Otago Schist: Comparisons to the Macraes DepositBy D Craw, L Cox, R J. Norris
The Rise and Shine Shear Zone is a mineralised low-angle deformation zone traceable for at least 7 km through biotite zone schist of the Dunstan Range, central Otago. The zone is commonly believed to
Jan 1, 2005