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Relevant bibliographies by topics / Division of Mines and Geology

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Academic literature on the topic 'Division of Mines and Geology'

Author: Grafiati

Published: 4 June 2021

Last updated: 1 February 2022

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Journal articles on the topic "Division of Mines and Geology"

1

Reitherman, Robert. "The Effectiveness of Fault Zone Regulations in California." Earthquake Spectra 8, no. 1 (February 1992): 57–77. http://dx.doi.org/10.1193/1.1585670.

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In 1990 a study was completed for the California Division of Mines and Geology on the effectiveness of California's fault zone regulations (the Alquist-Priolo Special Studies Zones Act and associated policies and activities). The Act, passed in 1972, instituted the following elements of a statewide mandatory approach to dealing with the hazard of surface fault rupture: state mapping of fault zones (Special Study Zones) where active faults are suspected; local government imposition of the requirement of a geologic study on new building projects within these Zones (with some single family dwellings and low-occupancy structures exempt); review procedures for the studies submitted by an applicant's geologist; prohibition of the siting of projects on active faults; notification of real estate purchasers that a property is located within a Zone. This paper presents the results of that evaluation and comments more broadly on applying the Alquist-Priolo model to other regions and to other geologic hazards.

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Brady, A. Gerald, and Anthony F. Shakal. "The Morgan Hill Earthquake of April 24, 1984—Strong-Motion Records." Earthquake Spectra 1, no. 3 (May 1985): 419–43. http://dx.doi.org/10.1193/1.1585274.

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Seventy-two strong-motion accelerograph stations, mostly from within the permanent networks of the U. S. Geological Survey and the California Division of Mines and Geology, were triggered during the Morgan Hill earthquake, April 24, 1984. Among the more interesting of the records are the large acceleration (1.29g) at Coyote Lake dam, the Gilroy array spanning the region between the San Andreas and Calaveras faults, the record from Hall's Valley (epicentral distance 4 km), and records from buildings, a bridge, and a dam within 20 km of the epicenter. Digitized data from 16 stations are available on tape.

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Brady, A. G., E. C. Etheredge, and R. L. Porcella. "The Whittier Narrows, California Earthquake of October 1, 1987—Preliminary Assessment of Strong Ground Motion Records." Earthquake Spectra 4, no. 1 (February 1988): 55–74. http://dx.doi.org/10.1193/1.1585465.

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More than 250 strong-motion accelerograph stations were triggered by the Whittier Narrows, California, earthquake of 1 October 1987. Considering the number of multichannel structural stations in the area of strong shaking, this set of records is one of the more significant in history. Three networks, operated by the U.S. Geological Survey, the California Division of Mines and Geology, and the University of Southern California produced the majority of the records. The excellent performance of the instruments in these and the smaller arrays is attributable to the quality of the maintenance programs and their funding and personnel requirements. Readiness for a magnitude 8 event is directly related to these maintenance programs. Prior to computer analysis of the analog film records, a number of important structural resonant modes can be identified, and frequencies and simple mode shapes have been scaled. The structural records form a basic performance measurement for comparison with larger earthquake response in the future.

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Stirling, Mark W., and Steven G. Wesnousky. "Comparison of recent probabilistic seismic hazard maps for southern California." Bulletin of the Seismological Society of America 88, no. 3 (June 1, 1998): 855–61. http://dx.doi.org/10.1785/bssa0880030855.

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Abstract Probabilistic seismic hazard (PSH) maps for southern California produced from the models of Ward (1994), the Working Group on California Earthquake Probabilities (1995), and the U.S. Geological Survey and California Division of Mines and Geology (Frankel et al., 1996; Petersen et al., 1996) show the peak ground accelerations predicted with each model to occur at 10% probability in 50 years, and the probability that 0.2 g will occur in 30 years, for “rock” site conditions. Differences among the maps range up to 0.4 g and 50%, respectively. We examine the locations and magnitudes of the differences as a basis to define the issues and avenues of research that may lead to more confident estimates of PSH in the future. Our analysis shows that three major factors contribute to the observed differences between the maps. They are the size of maximum magnitude assigned to a given fault, the proportion of predicted earthquakes that are distributed off the major faults, and the use of geodetic strain data to predict earthquake rates.

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Hou, En Ke, Jie Feng, Fan Yang, and Yan Jing Zhang. "Prediction of Groundwater Inrush into Coal Mines from Aquifers Overlying the First Coal Seam in Eastern Ningxia Coalfield, China." Advanced Materials Research 1073-1076 (December 2014): 1634–40. http://dx.doi.org/10.4028/www.scientific.net/amr.1073-1076.1634.

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In the region where Eastern Ningxia coalfield locates, with the fragile eco-environment and the relative short water resources, it is significant to make clear the influence of coal mining on the groundwater in this region. According to analyses of water-filling factors for the 21 mine fields in the 7 mining areas and 1 independent mine field of Eastern Ningxia coalfield. Firstly, this paper selects the formula in the regulations on the preserving of the coal pillar and coal mining under buildings, water, rail and main shafts (regulations for short) and the Standard on the Exploration of Hydrogeology and Engineering-Geology in the Mining Area (GB12719-91) (standard for short) to calculate the height of water-flow fractured zone in the first coal seam mining, and compares the analysis results of the above formula to the observation data of 3 working faces, and determine the estimated method on the height of water-flow fractured zone, and then use “three maps-two predictions” method to complete the criterion of aquifer water-enrichment and inbreak in safety of the first coal seam. Finally, analyzing the influence of coal mining on the direction of groundwater and recharge-runoff-discharge conditions, the final comprehensive division program on the risk of the groundwater inrush is presented. The research results served as the general guidelines for the mine operations.

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Brovender, Yurii, Hennadii Haiko, and Olena Brovender. "Mining under the early metal in the context of Kartamysh ore occurrence of Ukrainian Donbas." Mining of Mineral Deposits 15, no. 3 (September 2021): 45–53. http://dx.doi.org/10.33271/mining15.03.045.

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Purpose is to identify process engineering of mining under the Late Bronze age (18th-13th centuries BCE) in the context of copper deposits in the Eastern Ukraine. Among other things, it concerns analysis of manufacturing artifacts (i.e. ore production and preparation) in Kartamysh archeological area within the copper-ore territory of Bakhmut basin of Donbas. Methods. Following methods have been applied: a comparative historical method supported by typological archaeological approach; statistical procedures; engineering and geological methods to determine extraction volumes and evaluate copper ore extraction from the mines in Kartamysh archaeological area as well as structural and technologic analysis; functional and typological analysis; traceological analysis; experimental modelling; and carbon dating. Findings. Analysis of the specialized mining artifacts in Kartamysh archaeological area as well as mining artifacts within other copper-ore deposits in Bakhmut basin, extracted actively under the Late Bronze age, has made it possible to consider newly a number of important issues connected with process engineering of mining, specialization and labour division of ancient miners as well as evaluate significance of Donbas copper mines for the system of metal production development in the Eastern Europe of the second millennium BCE. Originality.Analysis of Kartamysh archaeological area, where the majority of business performance objects are connected with mining, has helped the authors consider specialization of the industrial systems (i.e. different-purpose mine workings, various mining tools, and areas to prepare ore) right from the viewpoint of the production method. Since similar situation is typical for other Donets complex artifacts, being involved in scientific terminology as the mining and smelting one, it would be more reasonable to represent it as Donets ore mining system owing to its specialization in the integrated copper ore extraction and preparation. Practical implications.The research results develop the history of mining science and engineering inclusive of ancient mining history in the Eastern Ukraine. They may be applied to train mining experts and in the process of creation of museum exhibitions (looking ahead, creation of Kartamysh skansen) while synthesizing technical and humanitarian aspects of engineering activities.

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Crouse, C. B., and Behnam Hushmand. "Soil-structure interaction at CDMG and USGS accelerograph stations." Bulletin of the Seismological Society of America 79, no. 1 (February 1, 1989): 1–14. http://dx.doi.org/10.1785/bssa0790010001.

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Abstract Forced harmonic and impulse-response vibration tests were conducted at several California accelerograph stations operated by the California Division of Mines and Geology (CDMG) and U.S. Geological Survey (USGS) to determine the extent to which soil-structure interaction may be affecting the recorded ground motions. The results of the tests on the foundations comprising USGS Station 6 in the Imperial Valley and CDMG Cholame 1E and Fault Zone 3 stations in the Cholame Valley indicated the presence of highly damped fundamental frequencies between 20 and 40 Hz. However, at the much larger Differential Array station, a masonry-block structure approximately 6 km southwest of Station 6, a moderately damped fundamental frequency of 12 Hz was observed. Approximate transfer functions between earthquake motions recorded at the stations and the free-field motions were computed from the response data obtained from the forced harmonic vibration tests. For the three smaller stations, these functions showed peak amplification factors ranging from 1.25 to 1.4 at frequencies between 20 and 40 Hz. The amplification at smaller frequencies was insignificant. For the Differential Array station, the amplification factor was 1.5 at 12 Hz and was roughly 0.6 for frequencies between 14 and 25 Hz. These results suggest that soil-structure interaction will have little effect on ground motions recorded at the smaller stations provided that most of the energy in these motions is confined to frequencies less than approximately 20 Hz. However, at the Differential Array station, soil-structure interaction probably has had, and will continue to have, a significant influence on the motions recorded at this station.

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Gellner, David N. "Language, caste, religion and territory: Newar identity ancient and modern." European Journal of Sociology 27, no. 1 (May 1986): 102–48. http://dx.doi.org/10.1017/s0003975600004549.

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The newars are the indigenous inhabitants of the Kathmandu Valley, a bowl-shaped plateau about fifteen miles across at a height of approximately 4,000 fest in the Himalayan foothills. It is a plateau in that the major rivers in the immediate area (the Trisuli and the Sunkosi) pass it by at a much lower level. The Valley is surrounded by a rampart of hills rising to 7 or 8,000 feet; according to local belief and myth, and according to geology, the Valley was once a lake. Its soil is exceptionally fertile by Himalayan, or indeed any, standards. Thanks to this, and to the Valley's strategic position astride trade routes to Tibet, it has a long and distinguished history. Written records (inscriptions) begin in the fifth century A.D. and give evidence of a high and literate civilization derived from the Indian plain. The inscriptions are written in a chaste and pure Sanskrit not met with in later periods, but the place-names reveal that the bulk of the population spoke an ancient form of the presentday Newars' language, Newari (Malla 1981 (1). Whereas most of the rest of Nepal remained thinly inhabited and rustic till the modern period, the Kathmandu Valley was able to support a division of labour and a sophisticated urban civilization impossible elsewhere in the Himalayan foothills between Kashmir and Assam.

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Beydik, O. "INDIGENOUS MINERAL DEPOSITS IN THE TABLE D. I. MENDELEEV: WORLD DIMENSION." Bulletin of Taras Shevchenko National University of Kyiv. Geography, no. 74 (2019): 13–17. http://dx.doi.org/10.17721/1728-2721.2019.74.3.

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Geography of mineral deposits and the distribution of chemical elements on the globe are characterized by heterogeneity. Mineral resources of the world, mineral deposits are devoted to a large array of publications of domestic and foreign specialists – geologists, geographers, geochemists, economists. During the mastering of the material, comparative-geographical, cartographic (analysis of maps of mineral resources, mineral resources in the context of continents and regions of the world), monographic (fundamental works of leading domestic and foreign geologists and resource scientists, geological and mineral reference books and dictionaries, multi-volume editions, devoted to the geology and mineral resources of individual countries and regions of the world) methods, systematic approach, in the processing and systematization of data used modern no computer technology. The explored deposits of mineral raw materials (actual and potential) form on the planet as separate local deposits, as well as geochemical zones – areas where concentrated economically valuable chemical elements and their compounds (minerals and rocks) are diverse in genesis (origin), stocks, exploitation possibilities. The largest of them are Appalachians in the USA – Western Hemisphere, High Velt in South Africa, Hibiny and Ural in Russia – Eastern Hemisphere. Leading countries in the territory where most of the geochemical raw materials are mined from the bowels are the USA (65 % of the total number of elements of the table), Russia (48 %), China (38 %), Canada (38 %), South Africa (30 %), Australia (27 %), Kazakhstan (19 %), India (14 %), Mexico (13 %). Systematized representations about the level of provision of mineral raw materials and minerals of individual countries and territories of the world. D. I. Mendeleev’s table and its mineral raw materials are presented as an objective factor of the international geographical division of labour. The given data reveal an adequate level of provision of countries and territories with mineral resources. The highlighted problem has confirmed the high density of interdisciplinary connections (geography, geology, geochemistry, economics, regionalisms). The given data can be implemented in the latest programs of reformed education in Ukraine.

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10

Touret, Lydie. "École des Mines." Rocks & Minerals 84, no. 3 (May 2009): 264–75. http://dx.doi.org/10.3200/rmin.84.3.264-275.

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Dissertations / Theses on the topic "Division of Mines and Geology"

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Lavoie, Sébastien. "Géologie de la mine East-Sullivan, Abitibi-Est, Val-d'or, Québec /." Thèse, Chicoutimi : Université du Québec à Chicoutimi, 2003. http://theses.uqac.ca.

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Holme, Philip J. "Quarternary geology and stratigraphy of the Beaver Mines map area, southwest Alberta." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1999. http://www.collectionscanada.ca/obj/s4/f2/dsk2/ftp03/MQ39833.pdf.

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Buckland, Adelene. "Truth lies hidden deep in Mines : Geology and the Victorian realist novel." Thesis, University of Oxford, 2008. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.503946.

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Rohrlach, Bruce D. "The structural geology and mineralization at the Reedy's Gold Mines, Murchison Goldfield, Western Australia /." Title page, abstract and contents only, 1987. http://web4.library.adelaide.edu.au/theses/09SB/09sbr739.pdf.

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Oswin, W. M. "Upper Devonian/lower carboniferous volcanism and mineralisation in the area east of the Rio Tinto mines, Iberian Pyrite Belt." Thesis, University of Southampton, 1987. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.375672.

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Hopper, Derek J. "Crustal evolution of paleo- to mesoproterozoic rocks in the Peake and Denison Ranges, South Australia /." [St. Lucia, Qld.], 2001. http://www.library.uq.edu.au/pdfserve.php?image=thesisabs/absthe18288.pdf.

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Twumasi, Frederick. "Applying MODFLOW and Artificial Neural Networks to Model the Formation of MinePools in Underground Coal Mines." Ohio University / OhioLINK, 2018. http://rave.ohiolink.edu/etdc/view?acc_num=ohiou1525989430737353.

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8

Noppé, Mark Adrian. "Geological controls for coal exploration and mining." Thesis, Rhodes University, 1992. http://hdl.handle.net/10962/d1005566.

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The identification and interpretation of geological features is essential for the planning and ultimate success of any mining venture. Examples of geological features significant for mining are presented, and their identification during exploration discussed. In particular, the importance of coal qualities, seam thickness and seam elevation are emphasised in relation to longwall mining. Geostatistical analysis provides a powerful tool for improving the prediction and decision-making capabilities of both exploration and mine geologists. The availability of geostatistics, and the benefits resulting from its application, are demonstrated using actual data for calorific value, seam thickness and seam elevation. Contamination of run-of-mine coal is a common problem on highly-mechanised collieries. The problem generally arises from over-cutting of the designated mining horizon. A practical system for monitoring and controlling contamination on a mechanised bord-and-pillar and longwall colliery is presented. The results and benefits of applying such a system are cited for an actual longwall colliery. Numerical geological predictions are not always reported in terms of the reliability of such estimates. Many of these values can be reported in terms of confidence limits, particularly for routine grade control purposes. The methods and benefits of such reporting are described and illustrated by way of examples for calorific value and contamination levels.

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9

Greene, Shane. "Noble gases of the Canadian Shield from the Lupin and Con Mines, Canada, as indicators of deep groundwater flow dynamics and residence time." Thesis, University of Ottawa (Canada), 2005. http://hdl.handle.net/10393/26917.

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Dissolved noble gas geochemistry provides insight on origin of saline groundwaters in two Canadian Shield mines, the Lupin and Con mines in Northern Canada. Within the Con major ion and isotope geochemistry indicate groundwaters from the deepest levels sampled remain relatively undisturbed by mining. Estimates of residence time for the Con mine brines, based on radiogenically produced helium and argon, indicate a Paleozoic age, consistent with recharge during the presence of Devonian seawater in this region. This is largely corroborated by krypton and xenon concentrations which reflect concentrated brine that has equilibrated with air before infiltration. Saline waters in the Lupin mine have an age of at least 130 Ma. At the Lupin mine, neon, krypton and xenon concentrations indicate degassing has occurred, likely caused by depressurization during mining along the V1 fault/fracture zone.

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Sperling, Antonin. "Slope stability and groundwater hydrology research for pitwall design at Equity Silver Mines Ltd., Houston, British Columbia." Thesis, University of British Columbia, 1985. http://hdl.handle.net/2429/25113.

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Structural geology, groundwater, shear strength and blasting control pitwall stability at Equity Silver Mines, Houston, British Columbia. A geotechnical investigation of, these parameters was carried out in the Main Zone pit during the summer of 1984. The objective of the study was to develop a pitwall design based on geologic and groundwater conditions observed in each design sector. This thesis presents the results of the investigation; methods of improving stability by drainage and control blasting are also discussed. Information on structural geology was obtained by line mapping of existing berms. The discodat package of computer programs was used to process the structural data and to identify trends in orientation of discontinuities. Based on this information, the Main Zone pit was divided into ten design sectors, each sector having a consistent pattern of discontinuity orientations, rock type, groundwater conditions and pit wall orientation. Kinematically possible failure modes were identified in each design sector. Failure modes that were expected to present stability problems were analyzed to calculate factor of safety. Pit wall and berm face angles were then selected such that only a small number of potential failure modes will daylight. The stability evaluation has shown that it should be possible to increase pitwall angles by 5〫 in the west half of the pit. However, the data base in this area of the pit is presently limited because only a small number of berms are exposed. Therefore, additional line mapping will be required before the west wall design can be finalized. Groundwater will reduce pitwall stability, especially in the east half of the Main Zone pit. Multi-berm failures are very sensitive to groundwater conditions. A dewatering system should be installed in the Main Zone pit to minimize the possibility of such failures occuring. Wet blastholes dictate that expensive water resistant slurry explosives be used in many areas of the Main Zone pit. The dewatering system should also draw down the water table so blastholes will become dryer and less expensive ANFO can be utilized. The magnitude of shear strength on failure surfaces is required in order to evaluate stability of potential failures. Slip tests, point load tests and back analyses of existing failures were used to determine the shear strength parameters. Further studies should be carried out to better define the parameters at higher stress levels that will develop in a multi-berm failure. Further potential for pit steepening exists if the berm face in the volcanics can be maintained at a slightly steeper angle, e.g. 70 instead of the present 66°. It may be possible to achieve this goal if trim blasting procedures are modified to reduce blast damage to the final wall.
Applied Science, Faculty of
Mining Engineering, Keevil Institute of
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Books on the topic "Division of Mines and Geology"

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H, Collins W. The geology of Gowganda mining division. Ottawa: Govt. Print. Bureau, 1997.

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H, Collins W. La géologie de la division minière de Gowganda. Ottawa: Impr. du gouvernement, 1997.

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Mines, Ontario Ministry of Northern Development and. Index to published report and maps: Mines and minerals division, 1891 to 1992. Toronto, Ont: Queen's Printer for Ontario, 1993.

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Survey, Ontario Geological. Index to published reports and maps, Mines and Minerals Division 1891 to 1992. Ontario: Ministry of Northern Development and Mines, 1993.

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5

Colorado. Office of State Auditor. Division of Minerals and Geology minerals program: Performance audit. [Denver, Colo: Office of State Auditor, 1993.

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McConnell, R. G. Portions of Portland Canal and Skeena mining divisions, Skeena District, B.C. Ottawa: Govt. Print. Bureau, 1997.

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Ontario. Ministry of Northern Development and Mines. Mines and Minerals Division. Mines and minerals division publictions price list = Division des mines et des mineraux prix des publications. Toronto, ON: Ministry of Northern Development and Mines, 1996.

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Exploring Idaho geology. Boise, Idaho: Mineral Land Publications, 1987.

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9

Division, Ontario Ministry of Northern Development and Mines Mines and Minerals. Call on us: Mines and Minerals Division, Ministry of Northern Development and Mines. Toronto, Ont: Ministry of Northern Development and Mines, 1987.

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Sheehan, William. Hearts & mines: The British 5th Division, Ireland, 1920-1922. Cork: Collins Press, 2009.

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Book chapters on the topic "Division of Mines and Geology"

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Vuks, V. Ja. "Lower and Middle Jurassic Stratigraphic Scheme of the Western Caucasus: Problems of Correlation and Division." In Springer Geology, 609–13. Cham: Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-04364-7_117.

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Marinos, Paul, Harry Saroglou, Mark Novack, Maria Benissi, and Vassilis Marinos. "Site Investigation for Abandoned Lignite Mines in Urban Environment." In Engineering Geology for Infrastructure Planning in Europe, 393–404. Berlin, Heidelberg: Springer Berlin Heidelberg, 2004. http://dx.doi.org/10.1007/978-3-540-39918-6_46.

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Craddock, Paul T. "Classical Geology and the Mines of the Greeks and Romans." In A Companion to Science, Technology, and Medicine in Ancient Greece and Rome, 197–216. Hoboken, NJ, USA: John Wiley & Sons, Inc., 2016. http://dx.doi.org/10.1002/9781118373057.ch12.

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Bekendam, Roland F. "Stability and Subsidence Assessment over Shallow Abandoned Room and Pillar Limestone Mines." In Engineering Geology for Infrastructure Planning in Europe, 657–70. Berlin, Heidelberg: Springer Berlin Heidelberg, 2004. http://dx.doi.org/10.1007/978-3-540-39918-6_73.

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Tămaș, Dan Mircea, Alexandra Tămaș, Alexander Magnus Jüstel, Martijn Passchier, Nils Chudalla, Lina Gotzen, Luis Alberto Pizano Wagner, et al. "A Field Guide to the Spectacular Salt Mines of the Transylvanian Basin and Romanian Carpathians." In Structural Geology and Tectonics Field Guidebook — Volume 1, 167–87. Cham: Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-60143-0_6.

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Lopes, Maria Eugénia, Maria José Afonso, José Teixeira, João P. Meixedo, J. Filinto Trigo, Maria João Dias Costa, Luís C. Gama Pereira, and Helder I. Chaminé. "Recovery of Ancient Groundwater Supply Systems and Old Abandoned Mines: Coupling Engineering Geosciences and Geoheritage Management." In Engineering Geology for Society and Territory - Volume 8, 227–30. Cham: Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-09408-3_37.

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Chowdhury, S., J. A. Mawer, P. Mukuka, and D. V. Stone. "Metallurgical circuit development and optimisation subsequent to commissioning of the tailings leach plant stage III at Nchanga Division of Zambia Consolidated Copper Mines Ltd, Zambia." In African Mining ’91, 299–307. Dordrecht: Springer Netherlands, 1991. http://dx.doi.org/10.1007/978-94-011-3656-3_29.

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"Subsidence over Old Mines." In Foundations of Engineering Geology, 72–73. CRC Press, 2018. http://dx.doi.org/10.1201/9781315273488-37.

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"Subsidence over Old Mines." In Foundations of Engineering Geology, 68–69. CRC Press, 2002. http://dx.doi.org/10.1201/9781482267785-32.

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"GEOLOGY OF CORNWALL: GRANITE, CLAY-SLATE, CHINA CLAY." In Cornwall, Its Mines and Miners, 70–77. Routledge, 2013. http://dx.doi.org/10.4324/9780203041758-23.

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Conference papers on the topic "Division of Mines and Geology"

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Adhikary, D. P., and H. Guo. "A Continuum Model for Simulating Mine Water Inflow and Gas Emission." In ASME 2008 Fluids Engineering Division Summer Meeting collocated with the Heat Transfer, Energy Sustainability, and 3rd Energy Nanotechnology Conferences. ASMEDC, 2008. http://dx.doi.org/10.1115/fedsm2008-55044.

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This paper describes a three-dimensional numerical model, called COSFLOW. It uses a Cosserat continuum approach for the efficient description of mechanical stress changes and deformation in weak layered rock, typical of coal measures. This mechanical model is coupled with a two-phase dual porosity fluid flow model to describe flow of water and gas through porous rock, desorption of gas from the matrix and subsequent flow of water and gas through the fracture network. The coupling includes simulation of permeability and porosity changes with rock deformation. Further the rock mass consisting of many interconnected fractures is idealized as an equivalent porous continuum using an equivalent anisotropic hydraulic conductivity matrix defined in terms of mean fracture spacing and mean aperture. This formulation is amenable to easy evaluation of modifications to the hydraulic conductivities as a function of stress induced changes in fracture aperture. The numerical code is used to simulate water inflow and gas emission in two Australian coal mines. The models at the two mine sites require significant geotechnical and hydrogeological data for adequate calibration. Many parameters in the model are not directly measurable and must be inferred by back-analysis of existing deformation, stress and hydrological data obtained during previous mining. The calibrated model is then used to make predictions for future mining panels. Water inflows at Mine A were predicted to increase significantly as mining progressed and this was supported by later measurements. This increase was attributed to wider longwall panels and increased roof rock permeability as more panels are mined. At Mine B, the model used measurements of gas production from predrainage boreholes for calibration and provided accurate predictions of average gas emissions into the longwall panel and post-drainage boreholes, although transient fluctuations were seen in the measurements. These were probably caused by local variations in geology or gas content or other factors not incorporated in the model.

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Krasniqi, Ramiz. "TAILING REFLOATING IN THE TREPCA MINES- PRISHTINA KOSOVO." In 14th SGEM GeoConference on SCIENCE AND TECHNOLOGIES IN GEOLOGY, EXPLORATION AND MINING. Stef92 Technology, 2014. http://dx.doi.org/10.5593/sgem2014/b13/s3.078.

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Hudecek, Vlastimil. "THE POSSIBILITY OF METHANE EXPLOATATION FROM CLOSED UNDEGROUND MINES." In 14th SGEM GeoConference on SCIENCE AND TECHNOLOGIES IN GEOLOGY, EXPLORATION AND MINING. Stef92 Technology, 2014. http://dx.doi.org/10.5593/sgem2014/b13/s3.090.

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Vuckovic, Bogoljub. "SULFUR IN LIGNITES OF KOLUBARA COAL MINES (KCM) � ENVIRONMENTAL FRIENDLY?" In 13th SGEM GeoConference on SCIENCE AND TECHNOLOGIES IN GEOLOGY, EXPLORATION AND MINING. Stef92 Technology, 2013. http://dx.doi.org/10.5593/sgem2013/ba1.v1/s03.069.

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Gibesova, Beata. "REDUCING DANGER OF COAL DUST IN COAL MINES IN CZECH REPUBLIC." In 13th SGEM GeoConference on SCIENCE AND TECHNOLOGIES IN GEOLOGY, EXPLORATION AND MINING. Stef92 Technology, 2013. http://dx.doi.org/10.5593/sgem2013/ba1.v1/s03.054.

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Manevski, Vladimir. "MODELS OF GEO-ELECTRICAL SOUNDING CHARACTERISTIC FOR COAL MINES (R. MACEDONIA)." In 13th SGEM GeoConference on SCIENCE AND TECHNOLOGIES IN GEOLOGY, EXPLORATION AND MINING. Stef92 Technology, 2013. http://dx.doi.org/10.5593/sgem2013/ba1.v2/s05.020.

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Bukowski, Przemyslaw. "CHANGES IN THE STRUCTURE OF WATER INFLOW INTO COAL MINES IN POLAND." In 13th SGEM GeoConference on SCIENCE AND TECHNOLOGIES IN GEOLOGY, EXPLORATION AND MINING. Stef92 Technology, 2013. http://dx.doi.org/10.5593/sgem2013/ba1.v2/s02.004.

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Hummelova, Ilona. "THE DETERMINATION OF THE PROTECTIVE LAYER ON THE REPOSITORIES OF URANIUM MINES." In 14th SGEM GeoConference on SCIENCE AND TECHNOLOGIES IN GEOLOGY, EXPLORATION AND MINING. Stef92 Technology, 2014. http://dx.doi.org/10.5593/sgem2014/b13/s3.084.

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Radu, Sorin Mihai. "ENERGETIC EFFICIENCY GROWTH OF COMPRESSED AIR DISTRIBUTION NETWORKS USED IN UNDERGROUND COAL MINES." In 13th SGEM GeoConference on SCIENCE AND TECHNOLOGIES IN GEOLOGY, EXPLORATION AND MINING. Stef92 Technology, 2013. http://dx.doi.org/10.5593/sgem2013/ba1.v1/s03.030.

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O’Connor, Chris, Luigi Cotesta, Richard Brummer, and Denis Thibodeau. "Non-linear modelling calibration process for Vale nickel mines Ontario division." In Fifth International Seminar on Deep and High Stress Mining. Australian Centre for Geomechanics, Perth, 2010. http://dx.doi.org/10.36487/acg_repo/1074_39.

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Reports on the topic "Division of Mines and Geology"

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van Staal, C. R. Geology, Caribou Mines, New Brunswick. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1994. http://dx.doi.org/10.4095/203261.

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van Staal, C. R. Geology, Brunswick Mines, New Brunswick. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1994. http://dx.doi.org/10.4095/203489.

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Holme, P. J. Surficial geology, Beaver Mines, Alberta. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1998. http://dx.doi.org/10.4095/209705.

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Lebel, D., and S. N. Hiebert. Geology, Beaver Mines, east half, Alberta. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2001. http://dx.doi.org/10.4095/212832.

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Batchelor, E. W. Geology of the Ptarmigan and Tom Mines. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/132315.

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Norris, D. K. Geology, Beaver Mines (west half), west of Fifth Meridian, Alberta-British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1993. http://dx.doi.org/10.4095/194042.

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Turner, R. J. W., R. G. Anderson, R. Franklin, L. Anderton, and F. Fowler. GeoTour guide for West Kootenay, British Columbia: geology, landscapes, mines, ghost towns, caves, and hot springs. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2009. http://dx.doi.org/10.4095/247599.

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Holme, P. H. J., S. R. Hicock, and L. E. Jackson. Quaternary geology and terrain inventory, Eastern Cordillera NATMAP Project. Report 5: stratigraphic correlations of glacial deposits in the Beaver Mines map area, southwestern Alberta. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1998. http://dx.doi.org/10.4095/209949.

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Holme, P. J. Quaternary geology and terrain inventory, eastern Cordillera NATMAP Project, Report 4: investigation of continental and montane advances in the Beaver Mines map area, southwestern Alberta. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1997. http://dx.doi.org/10.4095/208615.

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Solie, D. N., and L. E. Burns. Geology, geophysics, and geohazards along the Alaska Highway corridor, a project of the Alaska Division of Geological & Geophysical Surveys (poster): Yukon Geoscience Annual Convention, Whitehorse, November, 2006. Alaska Division of Geological & Geophysical Surveys, November 2006. http://dx.doi.org/10.14509/21842.

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