Academic literature on the topic 'Mining geophysics'

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Journal articles on the topic "Mining geophysics"

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Gochioco, Lawrence M., and Milovan Urosevic. "An introduction—Mining geophysics." Leading Edge 22, no. 6 (June 2003): 557. http://dx.doi.org/10.1190/1.1587677.

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Dębski, Wojciech. "Geophysics in geology and mining." Acta Geophysica 60, no. 2 (February 9, 2012): 384–85. http://dx.doi.org/10.2478/s11600-012-0014-z.

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Irvine, Richard. "Mining geophysics: A Canadian story." Preview 2019, no. 200 (May 4, 2019): 43. http://dx.doi.org/10.1080/14432471.2019.1621291.

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Mutton, Andrew J. "The application of geophysics during evaluation of the Century zinc deposit." GEOPHYSICS 65, no. 6 (November 2000): 1946–60. http://dx.doi.org/10.1190/1.1444878.

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During the period 1990 to 1995, experimental programs using high‐resolution geophysics at several Australian operating mines and advanced evaluation projects were undertaken. The primary aim of those programs was to investigate the application of geophysical technology to improving the precision and economics of the ore evaluation and extraction processes. Geophysical methods used for this purpose include: 1) borehole geophysical logging to characterize ore and rock properties more accurately for improved correlations between drill holes, quantification of resource quality, and geotechnical information. 2) imaging techniques between drill holes to map structure directly or to locate geotechnical problems ahead of mining. 3) high‐resolution surface methods to map ore contacts and variations in ore quality, or for geotechnical requirements. In particular, the use of geophysics during evaluation of the Century zinc deposit in northern Australia demonstrated the potential value of these methods to the problems of defining the lateral and vertical extent of ore, quantitative density determination, prediction of structure between drill holes, and geotechnical characterization of the deposit. An analysis of the potential benefit of using a combination of borehole geophysical logging and imaging suggested that a more precise structural evaluation of the deposit could be achieved at a cost of several million dollars less than the conventional evaluation approach based on analysis from diamond drill‐hole logging and interpolation alone. The use of geophysics for the Century evaluation also provided substance to the possibility of using systematic geophysical logging of blast holes as an integral part of the ore extraction process. Preliminary tests indicate that ore boundaries can be determined to a resolution of several centimeters, and ore grade can be estimated directly to a usable accuracy. Applying this approach routinely to production blast holes would yield potential benefits of millions of dollars annually through improved timeliness and accuracy of ore boundary and quality data, decreased dilution, and improved mill performance. Although the indications of substantial benefits resulting from the appropriate and timely use of geophysics at Rio Tinto’s mining operations are positive, some challenges remain. These relate largely to the appropriate integration of the technology with the mining process, and acceptance by the mine operators of the economic value of such work. Until the benefits are demonstrated clearly over time, the use of geophysics as a routine component of evaluation and mining is likely to remain at a low level.
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Asten, Michael. "Special Section on mining geophysics—Introduction." GEOPHYSICS 65, no. 6 (November 2000): 1851–61. http://dx.doi.org/10.1190/1.1444868.

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The Exploration 97 Conference held in Toronto in 1997 was a decennial event which provided a forum for review of advances in geophysics applied to mineral exploration and resource evaluation. This Special Section of Geophysics publishes a set of 16 papers, originally presented at that conference, which demonstrate recent advances in mineral exploration and mine geophysics.
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Gotovsuren, Uguumur, Amartuvshin Sodnomdorj, Khuukhnee Batdorj, Dashnvam Nergui, and Lawrence M. Gochioco. "Robust mining geophysics exploration in Mongolia." Leading Edge 31, no. 3 (March 2012): 304–6. http://dx.doi.org/10.1190/1.3694897.

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Legault, Jean, and Brendan Howe. "Introduction to this special section: Mining geophysics." Leading Edge 40, no. 2 (February 2021): 88. http://dx.doi.org/10.1190/tle40020088.1.

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Much has happened to the mineral exploration geophysics industry since TLE's last special section dedicated to mining geophysics was published in 2008. We are pleased to showcase the work of many talented mining geophysicists to the TLE readership in this issue's special section.
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Kuchin, Yan, and Jānis Grundspeņķis. "Machine Learning Methods for Identifying Composition of Uranium Deposits in Kazakhstan." Applied Computer Systems 22, no. 1 (December 1, 2017): 21–27. http://dx.doi.org/10.1515/acss-2017-0014.

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Abstract The paper explores geophysical methods of wells survey, as well as their role in the development of Kazakhstan’s uranium deposit mining efforts. An analysis of the existing methods for solving the problem of interpreting geophysical data using machine learning in petroleum geophysics is made. The requirements and possible applications of machine learning methods in regard to uranium deposits of Kazakhstan are formulated in the paper.
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Goodway, Bill. "Introduction to this special section: Mining geophysics." Leading Edge 31, no. 3 (March 2012): 288–90. http://dx.doi.org/10.1190/1.3694894.

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El Abidi El Alaoui, Meryeme, Latifa Ouadif, Lahcen Bahi, and Ahmed Manar. "Contribution of applied geophysics in mining prospecting." E3S Web of Conferences 150 (2020): 03016. http://dx.doi.org/10.1051/e3sconf/202015003016.

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The Eastern High Atlas (Morocco) contains a variety of rocks with different magnetic susceptibility, among these rocks are those which constitute the Proterozoic and Paleozoic basement of the plain of Tamlelt which is the study area. This work is devoted to the analysis and interpretation of the main magnetic anomalies using the Oisis Montaj program, and the correlation using ArcGis software, from the main « magnetic facies» detected, to the main geological formations affecting the geological basement, highlighted in the plain of Tamlelt. The map of the residual magnetic field shows elongated magnetic anomalies in the direction E-W and NE-SW. the reduction to the pole shows at the level of the plain of Tamlelt a large anomaly elongated in the direction E-W then in the direction NW-SE. The transformation of Tilt Angle allowed to delimit the anomalies of low or high amplitude that limit the shallow structures. The quantitative interpretation of the main magnetic anomalies highlighted in the study area has made it possible to characterize the deep structure of the magnetic bodies, which could contain sulphide clusters, according to the geological and mining context of the studied area.
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Dissertations / Theses on the topic "Mining geophysics"

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Sainoki, Atsushi. "Dynamic modelling of mining-induced fault-slip." Thesis, McGill University, 2014. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=123291.

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In deep hard rock mines where high stress conditions take place, rockbursts are serious problems because rockbursts could result in severe damage to mine openings. It is widely recognized that mining activities could reactivate faults in underground mines. The reactivation of faults could then cause fault-slip. More importantly, fault-slip gives rise to seismic waves, which inflict severe damage to mine openings. Because the generation and propagation of seismic waves are dynamic phenomena, fault-slip needs to be also dealt with as a dynamic phenomenon. Both of the static and dynamic behaviour of faults should be examined, considering the effects of mining activities on the faults, in order to estimate the damage induced by the seismic waves First, a literature review is conducted. The review has revealed that although a number of dynamic and static friction laws have been proposed, the friction laws have been rarely employed for the simulation of fault-slip in underground mines. The review has also revealed that most of the simulations have been conducted in static conditions. In this thesis, dynamic modelling of mining-induced fault-slip is presented using a mine-wide model encompassing a fault. Furthermore, a case study of Garson Mine, Sudbury, Canada is carried out. A parametrical study with a mine-wide 3D model has led to the following conclusions: (a) mining depth, friction angle of the fault, and fault locations exert a large influence on the maximum relative shear displacements on the fault, while the dilation angle and stiffness of the fault do not, (b) maximum slip rates appear to increase with the maximum slip. Results obtained from the numerical analysis employing Barton's shear strength model have shown that fault surface roughness strongly affects the intensity of seismic waves and seismically radiated energy. The results imply that fault-slip occurring on faults with rough surfaces could become more violent. The effect of stope production blasts on a nearby fault is also examined. The results obtained from the analysis have indicated that performing stope production blasts in timed sequence could induce a larger seismic event on the fault than triggering the blasts simultaneously. Dynamic analysis considering the collision and unloading of fault surface asperities is also conducted. It is found that the release of normal stress due to fault unloading has a large influence on the intensity of seismic waves. The effect of slip-weakening distance on seismic source parameters of fault-slip is also investigated. The study has indicated that slip rates and seismically radiated energy are significantly affected by the slip-weakening distance, while seismic moment appears not to be susceptible to the slip-weakening distance in a case of local fault-slip.Back analysis of fault-slip to estimate the physical and mechanical properties of shear/fracture zones is carried out for Garson Mine. The back analysis is conducted with respect to moment magnitude and peak particle velocities recorded by seismic monitoring systems. Fault surface roughness and a dynamic friction angle have been calibrated. Afterwards, the calibrated values are validated with peak ground acceleration. Through the study, a methodology to calibrate the physical and mechanical properties of faults by means of ground motion due to seismic waves arising from fault-slip as well as seismic source parameters of the fault-slip has been developed.
Dans les mines profondes ou des contraintes élevées se produisent, les coups de terrain sont un problème car les ils peuvent endommager les ouvertures minières. Il est largement reconnu que les activités minières peuvent réactiver des failles dans les mines sous-terraines. La réactivation de ces failles peut entrainer un glissement de faille. Surtout, le glissement de faille fait naitre des ondes sismiques qui infligent des dégâts sérieux quand elles frappent la surface des ouvertures minières. La génération et la propagation des ondes sismiques sont des phénomènes dynamiques. Il s'ensuit donc que le glissement de faille doit être traité comme un phénomène dynamique Le comportement dynamique ainsi que le comportement statique des failles doit être examiné en considérant les effets des activités minières pour estimer les dégâts causés par les ondes sismiques.Premièrement, un examen de la documentation est effectué. L'examen a révélé que même si un nombre de lois statiques et dynamiques de frottement ont été proposés, ces lois de frottement ont été peu employés pour simuler les glissements de faille que se déroulent dans les mines sous-terraines. La revue a aussi révélé que la majorité des simulations ont été conduites en conditions statiques. Dans cette thèse, la modélisation dynamique d'un glissement de faille induit par des activités minières est présentée. Le modèle englobe l'entièreté d'une mine. En plus, une étude de cas pour la mine Garson à Sudbury, au Canada, est effectuée.Une étude paramétrique avec un modèle de mine en trois dimensions mène aux conclusions suivantes: (a) la profondeur d'exploitation minière, l'angle de friction de la faille, et la position de la faille ont une grande influence sur les déplacement relatifs en cisaillement d'une faille, tandis que l'angle de dilation de la faille et la dureté ont peu d'effet, (b) le taux de glissement maximal augmente en fonction du glissement absolu. Les résultats obtenus du modèle numérique dans lequel le modèle de résistance au cisaillement de Barton est implémenté ont démontré que la rugosité de la surface de la faille affecte grandement l'intensité des ondes sismiques qui émanent du glissement de faille et l'énergie sismique propagée. Les résultats impliquent qu'un glissement de faille survenant à une faille rugueuse est plus violent. L'effet produit par un sautage de production sur une faille proche est aussi examiné en considérant plusieurs séquences de sautage. Les résultats de l'analyse indiquent qu'un sautage de production exécuté selon une séquence temporelle peut induire un plus grand événement sismique qu'un sautage simultané. Une analyse dynamique tenant compte la collision et le déchargement d'une faille est aussi conduite. Il est démontré que le relâchement de la contrainte normale à la faille a une grande influence sur l'intensité des ondes sismiques. L'effet de la distance d'affaiblissement de faille due glissement sur les paramètres sismiques est aussi examiné L'étude indique que le taux de glissement et l'énergie sismique émanée sont significativement affectés par la distance d'affaiblissement de faille, tandis que le moment sismique n'est pas susceptible à la distance d'affaiblissement dans le cas ou le glissement de faille se déroule seulement dans une zone limitée. Pour estimer l'effet des propriétés physiques et mécaniques de la zone de cisaillement, une analyse régressive est exécutée pour la mine Garson. L'analyse est conduite selon la magnitude du moment et la vitesse de crête des particules. La rugosité de la surface de la faille et l'angle de friction dynamique sont étalonnés. Ensuite, les paramètres étalonnés sont validés par rapport à l'accélération maximale du terrain. À travers l'étude, une méthodologie pour étalonner les propriétés physiques et mécaniques de la faille selon l'étude du mouvement du terrain due aux ondes sismiques émanant d'un glissement de faille est développé.
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Mlakar, Vincent William. "Crack development and acoustic emission studies in potash rock loaded under uniaxial compression." Thesis, McGill University, 1992. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=56670.

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Acoustic Emission (AE) techniques under laboratory testing conditions are used in order to understand the mechanical behavior and deformational processes of uniaxially compressed potash rock. Results obtained from the acoustic emission measurements are compared to crack development at preselected stress levels up to specimen failure.
It is observed that the fracture processes, mechanical behavior and acoustic emission response are dependent on the physical properties of potash rock. The mechanical behavior of potash rock displays two stress-strain trends under the same load conditions. Based on the acoustic emission rate, it was possible to delineate an approximate yield point of potash rock. However, a more detailed study of the acoustic emission amplitude and energy distributions showed that high amplitude events with long event durations are initially observed to occur near the yield point of the stress strain curves. These events are present prior to the yield point in specimens containing a high proportion of sylvite and after the yield point for monomineralic, halitic specimens. Finally, a classification scheme of crack morphology and systematic charts displaying the history of progressive crack development for all potash rock types has been developed.
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Priscu, Doina Maria. "Double-porosity modelling of groundwater flow through fractured rock masses." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1997. http://www.collectionscanada.ca/obj/s4/f2/dsk2/ftp01/MQ37280.pdf.

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Vukovic, Nikola. "Comparison of laboratory and field modulus of elasticity of rocks." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1998. http://www.collectionscanada.ca/obj/s4/f2/dsk1/tape11/PQDD_0001/MQ44047.pdf.

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Vander, Most Anastasia. "Recovery and analysis of historical mine data in a three-dimensional environment: A case study - Heath Steele, Bathurst Mining Camp, northern New Brunswick." Thesis, University of Ottawa (Canada), 2007. http://hdl.handle.net/10393/27927.

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3-D geographic information systems (GIS) provides a powerful tool for visualizing and interpreting the subsurface distribution of geology and hydrothermal parameters that are important in exploring for deposits concealed at depth. For the purpose of this study, restoration of a historical mine data set was undertaken with the goal of migrating information from paper records to fully linked data sets suitable for interpretation in 3-D GIS. Heath Steele, in the Bathurst Mining Camp, northern New Brunswick, is one such deposit with historical records that include the distribution of ore-associated iron formation, massive sulfides and host rocks. Structural and stratigraphic interpretations from previous studies and exploration programs were incorporated in the model, along with fabric measurements, regional geology, drillcore logs and geophysical data. This study shows how revisiting historical mine data in a 3-D environment can generate new knowledge about an ore deposit and particularly the spatial context of hydrothermal features in a complexly deformed setting that may aid future exploration.
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Alalawi, Saleh S. N., Salah S. H. Albehlany, Abdulaziz F. Aldossary, Rashid A. Alhashimi, Abdulsam M. Almurshidi, Laura L. Cathcart, Sherill L. Cole, et al. "Geophysical Surveys in the Pima Mining District, Arizona Volume I." LASI Laboratory for Advanced Surface Imaging, The University of Arizona (Tucson, AZ), 1989. http://hdl.handle.net/10150/624544.

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Geophysical surveys were conducted in the Pima mining district by students from the University of Arizona. The surveys were concentrated along section B-B' from Cooper (1973). The objectives of this survey included: teaching geophysical techniques, mapping regional structure along this profile, and determining which geophysical techniques were most useful for regional .mapping in this area. Controlled source audio-frequency magnetotelluric (CSAMT) surveys successfully mapped depth to basement along this profile. Seismic refraction surveys were not able to map depth to basement. Either the depth to basement was beyond the range of the arrays used in this experiment or there is insufficient contrast in the velocity between the basement and the overlying rocks. A test of the seismic reflection method was carried out using a walk-away noise spread. Possible reflections from basement were noted but were not sufficiently diagnostic to be routinely use able.
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Alalawi, Saleh S. N., Salah S. H. Albehlany, Abdulaziz F. Aldossary, Rashid A. Alhashimi, Abdulsam M. Almurshidi, Laura L. Cathcart, Sherill L. Cole, et al. "Geophysical Surveys in the Pima Mining District, Arizona Volume II." LASI Laboratory for Advanced Surface Imaging, The University of Arizona (Tucson, AZ), 1989. http://hdl.handle.net/10150/624550.

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Doucet, Chantale. "The effect of geology on fragmentation in small development headings." Thesis, McGill University, 1995. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=23744.

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This thesis presents the results of a research project on the effect of geology on the fragmentation of rock excavated by blasting in underground developments. The research was undertaken at CANMET's Experimental Mine in Val-d'Or, Quebec.
A total of thirteen (13) blasts were studied from November 1994 to February 1995. The analysis of each blast was divided into three stages: (1) Pre-blast: includes structural mapping, rockmass characterization, estimation of the in situ block size distribution and documentation of the blast design. (2) Blast: includes blast vibration monitoring and analysis. (3) Post-blast: includes determination of fragment size distribution, half-cast factors and bootlegs.
The blast design was kept as constant as possible throughout the study in order to limit the variation of parameters to the geology-related ones. The results were analyzed to determine any correlation between the rockmass characteristics and the blast results. Only general trends were found: (1) The characteristic size of the fragments obtained after blasting (x$ rm sb{c}$ blast) increases when the characteristic size of the in situ distribution (x$ rm sb{c}$ in situ) increases; (2) The characteristic size of the fragments obtained after blasting (x$ rm sb{c}$ blast) decreases when the adjusted powder factor increases; (3) The half-cast factor (HCF) decreases when the Rock Quality Designation (RQD), RMR and Q values increase; (4) The characteristic size of the fragments obtained after blasting (x$ rm sb{c}$ blast) increases when the RQD, Rock Mass Rating (RMR) and quality index (Q) values increase.
Some of these results confirm basic blasting principles whereas others were unexpected. The fact that no statistical correlation could be found is probably due to the geological environment in which the experiments were completed. The rock types encountered have very similar mechanical properties and the quality of the rockmasses did not vary extensively. Therefore, any variance in the results is best explained by the blast performance itself. (Abstract shortened by UMI.)
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Hadjigeorgiou, John. "A study of frictional properties of rock masses /." Thesis, McGill University, 1987. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=59612.

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The design of traditional and novel structures, e.g. underground tunnels, dam foundations, nuclear waste depositories, requires an understanding of the behaviour of rock under different stress conditions. This thesis is part of an overall research program into the behaviour of rock masses undertaken by the Department of Mining and Metallurgical Engineering at McGill University. The main objective of this project is the determination of the appropriate stress functions that describe the response of rock to applied loads. In this work, the distinction is made between intact, single discontinuity and fractured rock material.
The first segment of this thesis deals with a critical evaluation of the different failure criteria for rock and rock discontinuities that have been used in the past. Their applications and limitations are identified. In the second segment of this work, the frictional behaviour of rock and rock discontinuities is defined, based on results of laboratory testing in direct-shear and triaxial compression.
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Luo, Xiaochun. "Spatiotemporal stochastic models for earth science and engineering applications." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1998. http://www.collectionscanada.ca/obj/s4/f2/dsk1/tape11/PQDD_0016/NQ44665.pdf.

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Books on the topic "Mining geophysics"

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Idziak, Adam F. Geophysics in Mining and Environmental Protection. Berlin, Heidelberg: Springer-Verlag Berlin Heidelberg, 2011.

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Idziak, Adam F., and Ryszard Dubiel, eds. Geophysics in Mining and Environmental Protection. Berlin, Heidelberg: Springer Berlin Heidelberg, 2011. http://dx.doi.org/10.1007/978-3-642-19097-1.

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Canada, Geological Survey of. Borehole Geophysics For Mining and Geotechnical Applications. S.l: s.n, 1985.

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Jackson, M. J. 3DTOM, three-dimensional geophysical tomography. [Washington, D.C.?]: U.S. Dept. of the Interior, Bureau of Mines, 1996.

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Jackson, M. J. 3DTOM, three-dimensional geophysical tomography. [Washington, D.C.?]: U.S. Dept. of the Interior, Bureau of Mines, 1996.

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Jackson, M. J. 3DTOM, three-dimensional geophysical tomography. [Washington, D.C.?]: U.S. Dept. of the Interior, Bureau of Mines, 1996.

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Jackson, M. J. 3DTOM, three-dimensional geophysical tomography. [Washington, D.C.?]: U.S. Dept. of the Interior, Bureau of Mines, 1996.

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Jackson, M. J. 3DTOM, three-dimensional geophysical tomography. [Washington, D.C.?]: U.S. Dept. of the Interior, Bureau of Mines, 1996.

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Tweeton, Daryl R. BOMCRATR: A curved ray tomographic computer program for geophysical applications. Washington, D.C: U.S. Dept. of the Interior, Bureau of Mines, 1992.

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Idziak, Adam, and Ryszard Dubiel. Mining and environmental geophysics: Selected and revised contributions to the XXX Polish-Czech-Slovakian Symposium held at Lądek Zdrój on June 6-8, 2005. Warszawa: Instytut Geofizyki Polskiej Akademii Nauk, 2006.

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Book chapters on the topic "Mining geophysics"

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Eppelbaum, Lev, and Boris Khesin. "Mining Geophysics." In Lecture Notes in Earth System Sciences, 219–74. Berlin, Heidelberg: Springer Berlin Heidelberg, 2012. http://dx.doi.org/10.1007/978-3-540-76619-3_5.

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Alizadeh, Akif A., Ibrahim S. Guliyev, Fakhraddin A. Kadirov, and Lev V. Eppelbaum. "Mining Geophysics." In Geosciences of Azerbaijan, 281–311. Cham: Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-40493-6_8.

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Pfannkuch, H. O. "Medieval Saint Barbara Worship and Professional Traditions in Early Mining and Applied Earth Sciences." In History of Geophysics, 39–48. Washington, D. C.: American Geophysical Union, 2013. http://dx.doi.org/10.1029/hg003p0039.

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Kaláb, Zdeněk, and Jaromír Knejzlík. "Evaluation of Seismic Effects Generated by Mining Induced Seismic Events in Stonava Area." In Geophysics in Mining and Environmental Protection, 1–9. Berlin, Heidelberg: Springer Berlin Heidelberg, 2011. http://dx.doi.org/10.1007/978-3-642-19097-1_1.

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Idziak, Adam, and Iwona Stan-Kleczek. "The Use of Seismic Methods to Determine Potential Directions of Underground Water Flow in a Fractured Rock Mass." In Geophysics in Mining and Environmental Protection, 101–8. Berlin, Heidelberg: Springer Berlin Heidelberg, 2011. http://dx.doi.org/10.1007/978-3-642-19097-1_10.

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Vilhelm, Jan, Vladimír Rudajev, and Roman Živor. "Assessment of Fracture Properties from P-Wave Velocity Distribution." In Geophysics in Mining and Environmental Protection, 109–16. Berlin, Heidelberg: Springer Berlin Heidelberg, 2011. http://dx.doi.org/10.1007/978-3-642-19097-1_11.

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Wysowska, Anna, and Jolanta Pierwoła. "Electrical Resistivity Imaging Method in Investigating Post-Glacial Geomorphological Forms." In Geophysics in Mining and Environmental Protection, 117–25. Berlin, Heidelberg: Springer Berlin Heidelberg, 2011. http://dx.doi.org/10.1007/978-3-642-19097-1_12.

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Ćmiel, Stanisław Roman, and Maria Dziurowicz. "Frictional Metamorphism of Coal in the Upper Silesia Coal Basin, Southern Poland." In Geophysics in Mining and Environmental Protection, 127–33. Berlin, Heidelberg: Springer Berlin Heidelberg, 2011. http://dx.doi.org/10.1007/978-3-642-19097-1_13.

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Lizurek, Grzegorz, and Paweł Wiejacz. "Moment Tensor Solution and Physical Parameters of Selected Recent Seismic Events at Rudna Copper Mine." In Geophysics in Mining and Environmental Protection, 11–19. Berlin, Heidelberg: Springer Berlin Heidelberg, 2011. http://dx.doi.org/10.1007/978-3-642-19097-1_2.

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Kaláb, Zdeněk, and Markéta Lednická. "Seismic Loading of Medieval Jeroným Mine During West Bohemia Swarm in 2008." In Geophysics in Mining and Environmental Protection, 21–29. Berlin, Heidelberg: Springer Berlin Heidelberg, 2011. http://dx.doi.org/10.1007/978-3-642-19097-1_3.

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Conference papers on the topic "Mining geophysics"

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A. Sauck, William. "Mining Geophysics In The New Millenium." In 7th International Congress of the Brazilian Geophysical Society. European Association of Geoscientists & Engineers, 2001. http://dx.doi.org/10.3997/2214-4609-pdb.217.161.

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Pfaffhuber, Andi, Helgard Anschuetz, Hamed Rafezi, Alexandre Novo, Ferri P. Hassani, K. I. Sorensen, Weiqiang Liu, et al. "Airborne Geophysics, Remote Sensing, UAV (Drone)-based Surveys and Mining Geophysics." In Symposium on the Application of Geophysics to Engineering and Environmental Problems 2015. Society of Exploration Geophysicists and Environment and Engineering Geophysical Society, 2015. http://dx.doi.org/10.4133/sageep.28-005.

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Eppelbaum, Lev. "INFORMATION CONVOLUTION OF GEOPHYSICAL DATA: IMPLICATION IN MINING, PETROLEUM AND ARCHAEOLOGICAL GEOPHYSICS." In Symposium on the Application of Geophysics to Engineering and Environmental Problems 2015. Society of Exploration Geophysicists and Environment and Engineering Geophysical Society, 2016. http://dx.doi.org/10.4133/sageep.29-095.

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Salmanova, V. R., N. V. Bormotova, and Kulichkov V.P. "ОПЫТ ПРИМЕНЕНИЯ АЛГОРИТМОВ DATA MINING ДЛЯ ПОИСКОВ ЗАЛЕЖЕЙ НЕФТИ ГЕОХИМИЧЕСКИМИ МЕТОДАМИ." In Geophysics 2009. European Association of Geoscientists & Engineers, 2009. http://dx.doi.org/10.3997/2214-4609-pdb.319.35.

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Вакуленко, С. А., and С. В. Буряк. "Современные методы обработки морской инженерной сейсморазведки." In Engineering and Mining Geophysics 2018. Netherlands: EAGE Publications BV, 2018. http://dx.doi.org/10.3997/2214-4609.201800483.

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Виеццоли, A., A. Менгини, Г. Селф, and В. Ф. Каминский. "Месторождение Sunnyside: Калибровочная площадка для аэро ЭМ геофизических систем." In Engineering and Mining Geophysics 2018. Netherlands: EAGE Publications BV, 2018. http://dx.doi.org/10.3997/2214-4609.201800484.

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Куликов, В. А., С. В. Зайцев, and А. Г. Яковлев. "Современные электроразведочные технологии при поисках и разведке рудных месторождений." In Engineering and Mining Geophysics 2018. Netherlands: EAGE Publications BV, 2018. http://dx.doi.org/10.3997/2214-4609.201800485.

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Тригубович, Г. М., С. О. Шевчук, А. С. Сверкунов, and С. В. Барсуков. "Концепция построения автоматизированного навигационно-измерительного аэрогеофизического комплекса." In Engineering and Mining Geophysics 2018. Netherlands: EAGE Publications BV, 2018. http://dx.doi.org/10.3997/2214-4609.201800454.

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Шарафутдинов, Р. Ф., Р. А. Валиуллин, А. Ш. Рамазанов, В. Я. Федотов, and Д. В. Космылин. "Метод нестационарной «активной» термометрии при диагностике состояния скважин." In Engineering and Mining Geophysics 2018. Netherlands: EAGE Publications BV, 2018. http://dx.doi.org/10.3997/2214-4609.201800455.

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Колесников, В. П., and Т. А. Ласкина. "Мониторинг процессов соляного карстообразования методами электрометрии." In Engineering and Mining Geophysics 2018. Netherlands: EAGE Publications BV, 2018. http://dx.doi.org/10.3997/2214-4609.201800456.

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Reports on the topic "Mining geophysics"

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Killeen, P. G. Borehole geophysics for mining and geotechnical applications. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1986. http://dx.doi.org/10.4095/123596.

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Tschirhart, P. A., and W. A. Morris. Integration of rock properties and geophysics, Bathurst Mining Camp. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2015. http://dx.doi.org/10.4095/296547.

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Mwenifumbo, C. J., and A. L. Mwenifumbo. Borehole geophysical logging in the Flin Flon mining camp. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2012. http://dx.doi.org/10.4095/291534.

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Burns, L. E., A. M. Emond, and G. R. C. Graham. Fortymile mining district electromagnetic and magnetic airborne geophysical survey, data compilation. Alaska Division of Geological & Geophysical Surveys, June 2015. http://dx.doi.org/10.14509/29411.

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Burns, L. E., A. M. Emond, and G. R. C. Graham. Livengood mining district electromagnetic and magnetic airborne geophysical survey, data compilation. Alaska Division of Geological & Geophysical Surveys, May 2015. http://dx.doi.org/10.14509/29412.

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Burns, L. E., and G. R. C. Graham. Petersville mining district electromagnetic and magnetic airborne geophysical survey, data compilation. Alaska Division of Geological & Geophysical Surveys, June 2015. http://dx.doi.org/10.14509/29445.

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Burns, L. E., G. R. C. Graham, and A. M. Emond. Bonnifield mining district electromagnetic and magnetic airborne geophysical survey, data compilation. Alaska Division of Geological & Geophysical Surveys, 2016. http://dx.doi.org/10.14509/29557.

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Thomas, M. D., J. A. Walker, P. Keating, R. Shives, F. Kiss, and W. D. Goodfellow. Geophysical atlas of massive sulphide signatures Bathurst mining camp, New Brunswick. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2000. http://dx.doi.org/10.4095/211549.

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Puchner, C. C., G. M. Smith, R. W. Flanders, D. E. Crowe, S. C. McIntyre, and L. E. Burns. Combined geology and airborne geophysical data of the Ruby-Poorman mining district, Alaska. Alaska Division of Geological & Geophysical Surveys, 1998. http://dx.doi.org/10.14509/1876.

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Athey, J. E., L. K. Freeman, C. P. Hults, D. J. Szumigala, M. B. Werdon, R. D. Koehler, and L. E. Burns. Update on geological and geophysical investigations in the Slate Creek mining area, Alaska (presentation). Alaska Division of Geological & Geophysical Surveys, November 2009. http://dx.doi.org/10.14509/29491.

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