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Journal articles on the topic 'Mineralogy'

Author: Grafiati

Published: 4 June 2021

Last updated: 25 July 2025

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1

Hoppe, G. "Zur Geschichte der Geowissenschaften im Museum für Naturkunde zu Berlin Teil 4: Das Mineralogische Museum der Universität Berlin unter Christian Samuel Weiss von 1810 bis 1856." Fossil Record 4, no. 1 (2001): 3–27. http://dx.doi.org/10.5194/fr-4-3-2001.

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Die Universitätsgründung in Berlin von 1810 war verbunden mit der Übernahme des Lehrbetriebes der aufgelösten Bergakademie, die nur noch in Form des Bergeleveninstituts bzw. Bergelevenklasse für die Finanzierung der Ausbildung der Bergeleven weiter bestand, sowie mit der Übernahme des von der Bergakademie genutzten Königlichen Mineralienkabinetts der preußischen Bergverwaltung als Mineralogisches Museum der Universität. Infolge des Todes von D. L. G. Karsten im Jahre 1810 erhielt der Leipziger Physiker und Mineraloge C. S. Weiss den Lehrstuhl für Mineralogie, den er bis zu seinem Tode 1856 inn

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2

Valsami-Jones, E., D. A. Polya, and K. Hudson-Edwards. "Environmental mineralogy, geochemistry and human health." Mineralogical Magazine 69, no. 5 (2005): 615–20. http://dx.doi.org/10.1180/s0026461x00045473.

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This issue of Mineralogical Magazine is the 5th in a loosely defined series of special thematic issues (or part issues), deriving from conferences organized by the Mineralogical Society. The associated conference was entitled ‘Environmental Mineralogy, Geochemistry and Human Health’ and took place in January 2005, in Bath. A common thread to all these Mineralogical Society conferences has been the role of mineralogy in applied science and technology and particularly in environmental science, focussing on the multidisciplinarity of modern mineralogy; the conferences (and special issues) have be

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3

Graham, Shaun, and Nynke Keulen. "Nanoscale Automated Quantitative Mineralogy: A 200-nm Quantitative Mineralogy Assessment of Fault Gouge Using Mineralogic." Minerals 9, no. 11 (2019): 665. http://dx.doi.org/10.3390/min9110665.

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Effective energy-dispersive X-ray spectroscopy analysis (EDX) with a scanning electron microscope of fine-grained materials (submicrometer scale) is hampered by the interaction volume of the primary electron beam, whose diameter usually is larger than the size of the grains to be analyzed. Therefore, mixed signals of the chemistry of individual grains are expected, and EDX is commonly not applied to such fine-grained material. However, by applying a low primary beam acceleration voltage, combined with a large aperture, and a dedicated mineral classification in the mineral library employed by t

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4

Kokkaliari, Maria, and Ioannis Iliopoulos. "Application of Near-Infrared Spectroscopy for the identification of rock mineralogy from Kos Island, Aegean Sea, Greece." Bulletin of the Geological Society of Greece 55, no. 1 (2020): 290. http://dx.doi.org/10.12681/bgsg.20708.

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Near-Infrared spectroscopy (NIR) is a useful tool for direct and on-site identification of rock mineralogy in spite of the difficulties arising in spectral evaluation, due to limited availability of spectral libraries at the time. Especially in the field, a functional methodology for the identification and evaluation if possible, of the geologic materials, is of interest to many researchers. However, several different parameters (such as grain size, color, mineralogy, texture, water content etc.) can affect the spectroscopic properties of the samples resulting in spectral variability. The subj

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5

Gutmann, J. "Mineralogy." Eos, Transactions American Geophysical Union 79, no. 27 (1998): 320. http://dx.doi.org/10.1029/98eo00242.

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6

Naldrett, A. J. "Mineralogy is alive." European Journal of Mineralogy 12, no. 1 (2000): 5–6. http://dx.doi.org/10.1127/ejm/12/1/0005.

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7

Dunham, A. C. "Developments in industrial mineralogy: II. Archaeological mineralogy." Proceedings of the Yorkshire Geological Society 49, no. 2 (1992): 105–15. http://dx.doi.org/10.1144/pygs.49.2.105.

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8

Okrusch, Martin, and Hans Ulrich Bambauer. "From the Fortschritte der Mineralogie to the European Journal of Mineralogy: a case history." European Journal of Mineralogy 22, no. 6 (2010): 897–908. http://dx.doi.org/10.1127/0935-1221/2010/0022-2047.

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9

Rakovan, John. "Environmental Mineralogy." Rocks & Minerals 83, no. 2 (2008): 172–75. http://dx.doi.org/10.3200/rmin.83.2.172-175.

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10

MATSUBARA, Satoshi. "Descriptive Mineralogy." Japanese Magazine of Mineralogical and Petrological Sciences 32, no. 3 (2003): 126–27. http://dx.doi.org/10.2465/gkk.32.126.

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11

Putirka, Keith D. "Exoplanet Mineralogy." Reviews in Mineralogy and Geochemistry 90, no. 1 (2024): 199–257. http://dx.doi.org/10.2138/rmg.2024.90.07.

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12

Kotova, O. B., and A. V. Ponaryadov. "Nanotechnological mineralogy." Journal of Mining Science 45, no. 1 (2009): 93–98. http://dx.doi.org/10.1007/s10913-009-0012-y.

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13

Bain, D. C. "Optical mineralogy." Earth-Science Reviews 24, no. 4 (1987): 284–85. http://dx.doi.org/10.1016/0012-8252(87)90068-7.

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14

Pernklau, Ernst. "Optical mineralogy." Chemical Geology 56, no. 3-4 (1986): 335. http://dx.doi.org/10.1016/0009-2541(86)90013-6.

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15

Escolme, Angela, Ron F. Berry, Julie Hunt, Scott Halley, and Warren Potma. "Predictive Models of Mineralogy from Whole-Rock Assay Data: Case Study from the Productora Cu-Au-Mo Deposit, Chile." Economic Geology 114, no. 8 (2019): 1513–42. http://dx.doi.org/10.5382/econgeo.2019.4650.

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Abstract Mineralogy is a fundamental characteristic of a given rock mass throughout the mining value chain. Understanding bulk mineralogy is critical when making predictions on processing performance. However, current methods for estimating complex bulk mineralogy are typically slow and expensive. Whole-rock geochemical data can be utilized to estimate bulk mineralogy using a combination of ternary diagrams and bivariate plots to classify alteration assemblages (alteration mapping), a qualitative approach, or through calculated mineralogy, a predictive quantitative approach. Both these techniq

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16

Fang, Qian, Hanlie Hong, Lulu Zhao, Stephanie Kukolich, Ke Yin, and Chaowen Wang. "Visible and Near-Infrared Reflectance Spectroscopy for Investigating Soil Mineralogy: A Review." Journal of Spectroscopy 2018 (2018): 1–14. http://dx.doi.org/10.1155/2018/3168974.

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Clay minerals are the most reactive and important inorganic components in soils, but soil mineralogy classifies as a minor topic in soil sciences. Revisiting soil mineralogy has been gradually required. Clay minerals in soils are more complex and less well crystallized than those in sedimentary rocks, and thus, they display more complicated X-ray diffraction (XRD) patterns. Traditional characterization methods such as XRD are usually expensive and time-consuming, and they are therefore inappropriate for large datasets, whereas visible and near-infrared reflectance spectroscopy (VNIR) is a quic

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17

van Hullebusch, Eric, and Stephanie Rossano. "Mineralogy, environment and health." European Journal of Mineralogy 22, no. 5 (2010): 627. http://dx.doi.org/10.1127/0935-1221/2010/0022-2064.

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18

Shchiptsov, V. V. "Technological mineralogy: from Academician V. M. Severgin to the present day." Vestnik of Geosciences 4 (2021): 20–24. http://dx.doi.org/10.19110/geov.2021.4.3.

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It is shown that the origins of technological mineralogy in Russia are associated with the name of Academician V. M. Severgin, who at the end of the 18th century introduced the concept of «technological and economic» mineralogy. The stage of development of 1921—1955 is considered as important for the formation of the school of applied mineralogy. The next stage is the implementation of the principles of technological mineralogy in the practice of geological exploration and mining production and the creation of the Technological Mineralogy Commission of the All-Union Mineralogical Society by th

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19

Paykov, Oksana, and Harmonie Hawley. "Property-based assessment of soil mineralogy using mineralogy charts." Applied Clay Science 104 (February 2015): 261–68. http://dx.doi.org/10.1016/j.clay.2014.12.003.

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20

Martinez, Alex, and Alan P. Byrnes. "Modeling Dielectric-constant Values of Geologic Materials: An Aid to Ground-penetrating Radar Data Collection and Interpretation." Bulletin (Kansas Geological Survey), no. 247 (January 1, 2001): 1–16. https://doi.org/10.17161/kgsbulletin.no.247.20391.

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Ground-penetrating radar (GPR) is a near-surface geophysical imaging technique used for non-intrusive subsurface geologic and engineering investigations. Dielectric constant is a critical parameter for GPR surveys because it controls propagation velocity of electromagnetic waves through material, reflection coefficients across interfaces of different materials, and vertical and horizontal imaging resolution. Dielectric constant in rocks and sediments is primarily a function of mineralogy, porosity, pore fluids, frequency, geometries, and electrochemical interactions between rock components. Re

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21

Matkovskyi, Orest, and Yevheniia Slyvko. "Academician Yevhen Lazarenko scientific readings and their contribution to the development of modern mineralogy." Mineralogical Collection 71, no. 1 (2021): 3–27. http://dx.doi.org/10.30970/min.71.01.

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Periodic Scientific Readings named after Academician Yevhen Lazarenko were offered by his students and followers from the Department of Mineralogy of Ivan Franko National University of Lviv and Ukrainian Mineralogical Society. The corresponding decision was made by the participants of the scientific conference (1997) dedicated to the 80th anniversary of Ye. Lazarenko. After all, perpetuating the memory of outstanding scientists and assessing the importance of their contribution to the development of basic science is impossible without scientific forums organized in their honour. Eleven such Sc

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22

SUGIYAMA, Kazumasa, and Akihiko NAKATSUKA. "Mineralogy and Crystallography." Nihon Kessho Gakkaishi 56, no. 3 (2014): 149. http://dx.doi.org/10.5940/jcrsj.56.149.

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23

Щипцов, Владимир Владимирович, Ольга Борисовна Котова, Елена Германовна Ожогина, et al. "TECHNOLOGICAL MINERALOGY COMPREHENSIVELY." Proceedings of the Karelian Research Centre of the Russian Academy of Sciences, no. 10 (October 26, 2021): 44. http://dx.doi.org/10.17076/geo1481.

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24

MURAKAMI, Takashi. "Reactions in mineralogy." Japanese Magazine of Mineralogical and Petrological Sciences 32, no. 3 (2003): 161–64. http://dx.doi.org/10.2465/gkk.32.161.

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25

Knittle, Elise. "Introduction to Mineralogy." Eos, Transactions American Geophysical Union 81, no. 34 (2000): 389. http://dx.doi.org/10.1029/00eo00292.

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26

Bloodworth, Andrew. "Mineralogy: Painful extractions." Nature 517, no. 7533 (2015): 142–43. http://dx.doi.org/10.1038/517142a.

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27

Butcher, Alan R. "Applied Mineralogy ’03." Minerals Engineering 16, no. 6 (2003): 571. http://dx.doi.org/10.1016/s0892-6875(03)00144-4.

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28

Downs, James W. "Manual of mineralogy." Geochimica et Cosmochimica Acta 59, no. 9 (1995): 1901. http://dx.doi.org/10.1016/0016-7037(95)90150-7.

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29

TOKONAMI, Masayasu. "Applications for mineralogy." Hyomen Kagaku 7, no. 1 (1986): 117–20. http://dx.doi.org/10.1380/jsssj.7.117.

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30

Vaughan, David J., and Claire L. Corkhill. "Mineralogy of Sulfides." Elements 13, no. 2 (2017): 81–87. http://dx.doi.org/10.2113/gselements.13.2.81.

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31

Haggerty, Stephen E. "Upper mantle mineralogy." Journal of Geodynamics 20, no. 4 (1995): 331–64. http://dx.doi.org/10.1016/0264-3707(95)00016-3.

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32

Dunham, A. C. "Developments in industrial mineralogy: I. The mineralogy of brick-making." Proceedings of the Yorkshire Geological Society 49, no. 2 (1992): 95–104. http://dx.doi.org/10.1144/pygs.49.2.95.

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33

Passaglia, Elio, and Ermanno Galli. "Natural zeolites: mineralogy and applications." European Journal of Mineralogy 3, no. 4 (1991): 637–40. http://dx.doi.org/10.1127/ejm/3/4/0637.

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34

Artioli, Gilberto, and Ivana Angelini. "Mineralogy and archaeometry: fatal attraction." European Journal of Mineralogy 23, no. 6 (2011): 849–55. http://dx.doi.org/10.1127/0935-1221/2011/0023-2119.

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35

Zhang, Qiong, and Jean-Baptist Peyaud. "Development and Validation of a Novel Interpretation Algorithm for Enhanced Resolution of Well Logging Signals." Journal of Sensors 2021 (January 7, 2021): 1–10. http://dx.doi.org/10.1155/2021/6610806.

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This work presents a novel algorithm that achieves enhanced resolution of well logging signals, e.g., from 1 ft of a pulsed neutron mineralogy tool to 0.04 ft of an imaging tool. The algorithm, denoted as “Digital Core,” combines mineralogical and sedimentological information to generate a high-resolution record of the formation mineralogy which can be consequently applied to thin bedded environments. The keystone to the philosophy of this algorithm is that the spectral information recorded by mineralogy tool is a weighted average of the mineralogy of each lithological component in the analyze

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36

Guntoro, Pratama Istiadi, Yousef Ghorbani, and Jan Rosenkranz. "3D Ore Characterization as a Paradigm Shift for Process Design and Simulation in Mineral Processing." BHM Berg- und Hüttenmännische Monatshefte 166, no. 8 (2021): 384–89. http://dx.doi.org/10.1007/s00501-021-01135-w.

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AbstractCurrent advances and developments in automated mineralogy have made it a crucial key technology in the field of process mineralogy, allowing better understanding and connection between mineralogy and the beneficiation process. The latest developments in X‑ray micro-computed tomography (µCT) have shown a great potential to let it become the next-generation automated mineralogy technique. µCT’s main benefit lies in its capability to allow 3D monitoring of the internal structure of the ore sample at resolutions down to a few hundred nanometers, thus excluding the common stereological erro

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37

Zhang, Qiong, and Jean-Baptist Peyaud. "Development and Validation of a Novel Interpretation Algorithm for Enhanced Resolution of Well Logging Signals." Journal of Sensors 2021 (January 7, 2021): 1–10. http://dx.doi.org/10.1155/2021/6610806.

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This work presents a novel algorithm that achieves enhanced resolution of well logging signals, e.g., from 1 ft of a pulsed neutron mineralogy tool to 0.04 ft of an imaging tool. The algorithm, denoted as “Digital Core,” combines mineralogical and sedimentological information to generate a high-resolution record of the formation mineralogy which can be consequently applied to thin bedded environments. The keystone to the philosophy of this algorithm is that the spectral information recorded by mineralogy tool is a weighted average of the mineralogy of each lithological component in the analyze

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38

Bhattacharyya, T., D. K. Pal, and S. B. Deshpande. "On kaolinitic and mixed mineralogy classes of shrink - swell soils." Soil Research 35, no. 6 (1997): 1245. http://dx.doi.org/10.1071/s96115.

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Spatially associated red (Typic Hapludalf) and black (Vertic Eutropept) soils developed on the Deccan plateau in the Western Ghats of India were analysed for clay mineralogy and also physical properties relating to shrink–swell. This was done in order to examine a possible correlation between shrink–swell phenomena and the content of expansible clay minerals, and to reconcile the apparent incompatibility between such a correlation and the classification of some Vertisols into kaolinitic, illitic, and mixed mineralogy classes. The fine clay mineralogy of the red soil was dominated by interstrat

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39

Burns, Roger G. "Spectroscopic Methods in Mineralogy and Geology reviews in mineralogy, vol. 18." Geochimica et Cosmochimica Acta 54, no. 1 (1990): 253. http://dx.doi.org/10.1016/0016-7037(90)90214-6.

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40

Naumko, I. M. "FINAL EDITION ON THE HISTORY OF MINERALOGY AND MINERALOGICAL KNOWLEDGE IN UKRAINE." Geological Journal, no. 2 (June 26, 2023): 68–74. http://dx.doi.org/10.30836/igs.1025-6814.2023.2.275507.

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Information on the history of mineralogical research and knowledge in the independent Ukraine (since 1991) іs summarized in the book. The world-famous scientific schools formed in the second half of the 20th century (1940–1990): regional mineralogical, thermobarogeochemical, crystallochemical, mineral physics are characterized. The achievements of scientists in regional, systematic and genetic mineralogy, crystal chemistry and mineral physics, mineralogical crystallography, bio- and nano-mineralogy, experimental, space and applied mineralogy, museum work, etc. were analyzed. It is shown that a

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41

Aldis, Margot, Maximilian Posch, and Julian Aherne. "Normative Mineralogy of 1170 Soil Profiles across Canada." Minerals 13, no. 4 (2023): 544. http://dx.doi.org/10.3390/min13040544.

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Weathering of soil minerals provides base cations that buffer against acidity, and nutrients that support plant growth. In general, direct observations of soil minerals are rare; however, their abundance can be determined indirectly through soil geochemistry using normative-calculation procedures. This study compiled a data set of major oxide content from published and archived soil geochemical observations for 1170 sites across Canada (averaged over the soil profile [A, B, and C horizons], weighted by depth and bulk density to a maximum depth of 50 cm). Quantitative soil mineralogy (wt%) was

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42

Keulen, Nynke, Sebastian Næsby Malkki, and Shaun Graham. "Automated Quantitative Mineralogy Applied to Metamorphic Rocks." Minerals 10, no. 1 (2020): 47. http://dx.doi.org/10.3390/min10010047.

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The ability to apply automated quantitative mineralogy (AQM) on metamorphic rocks was investigated on samples from the Fiskenæsset complex, Greenland. AQM provides the possibility to visualize and quantify microstructures, minerals, as well as the morphology and chemistry of the investigated samples. Here, we applied the ZEISS Mineralogic software platform as an AQM tool, which has integrated matrix corrections and full quantification of energy dispersive spectrometry data, and therefore is able to give detailed chemical information on each pixel in the AQM mineral maps. This has been applied

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43

Callen, Joaquim. "Topographic mineralogy and the book "Minerales y Minas de España"." Mineral Up 5, no. 3 (2019): 74–78. https://doi.org/10.5281/zenodo.3633613.

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Commentary on the classic books of national topographic mineralogies, and the book "Minerals and Mines of Spain", on the topographic mineralogy of Spain, by Miguel Calvo, and which has been published in nine volumes between 2003 and 2018

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44

Kratochvíl, Bohumil. "History of the Department of Solid State Chemistry, University of Chemistry and Technology, Prague." Chemické listy 119, no. 4 (2025): 181–93. https://doi.org/10.54779/chl20250181.

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The history of the Department of Solid State Chemistry at the University of Chemistry and Technology, Prague, dates back to 1835, when the position of Professor of natural sciences and commodities was created at the Prague Polytechnic and the eponymous Department was founded along with it. After division of the Polytechnic into Czech and German parts (1869), the position of Professor for mineralogy, geology and palaeontology and the corresponding Department for Mineralogy and Geology were established in the Czech part. In 1919, mineralogy was separated from geology at the Czech Technical Unive

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45

Palyanov, Yu N., and A. I. Nepomnyashchikh. "Modern Problems of Experimental Mineralogy, Petrology, and Geochemistry." Russian Geology and Geophysics 64, no. 8 (2023): 889–91. http://dx.doi.org/10.2113/rgg20234631.

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Abstract —This Special issue of Russian Geology and Geophysics is a collection of papers on current problems of experimental mineralogy, petrology, and geochemistry discussed at the XVIII Russian Conference on Experimental Mineralogy (5–10 September 2022, Vinogradov Institute of Geochemistry, Irkutsk). The scope of considered issues ranges from laboratory modeling of mineral formation processes in different tectonic settings to technical mineralogy. The reported experiments are run at pressures and temperatures corresponding to crustal and mantle conditions.

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46

Kittridge, Mark G. "Investigating the influence of mineralogy and pore shape on the velocity of carbonate rocks: Insights from extant global data sets." Interpretation 3, no. 1 (2015): SA15—SA31. http://dx.doi.org/10.1190/int-2014-0054.1.

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Using a variety of recent public-domain data sets comprising porosity, velocity (P- and S-waves), and, in most cases, mineralogy and petrographic data, I created an extensive global data set and evaluated the importance of mineralogy and pore type on the elastic properties behavior of carbonate core plugs. Results from this investigation clearly illuminated the potential for overinterpreting elastic properties behavior as a function of pore type(s) when mineralogy was not explicitly included in the analysis. Rock-physics analysis using a combination of heuristic and theoretical models illustra

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47

Shi, Yuchen, Jun Wang, Hongfei Ba, et al. "Process-Mineralogy-Guided Flotation for Cu-Co Recovery: A Case Study of DRC Copper–Cobalt Sulfide Ore." Processes 13, no. 3 (2025): 918. https://doi.org/10.3390/pr13030918.

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Process mineralogy is an important technique to evaluate the economic value of ore, and it also has an important guiding role in flotation. Copper–cobalt sulfide ore, a significant source of copper and cobalt metals, is abundant in the Democratic Republic of the Congo (DRC). In this paper, DRC copper–cobalt sulfide ore is employed to validate process mineralogy guidance for flotation, thereby enhancing Cu-Co recovery. Process mineralogy results indicate that the economically valuable metals in copper–cobalt sulfide ore are Cu and Co. Cu is predominantly deposited in chalcopyrite, bornite, chal

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48

Stoll, Nicolas, Maria Hörhold, Tobias Erhardt, Jan Eichler, Camilla Jensen, and Ilka Weikusat. "Microstructure, micro-inclusions, and mineralogy along the EGRIP (East Greenland Ice Core Project) ice core – Part 2: Implications for palaeo-mineralogy." Cryosphere 16, no. 2 (2022): 667–88. http://dx.doi.org/10.5194/tc-16-667-2022.

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Abstract. Impurities in polar ice do not only allow the reconstruction of past atmospheric aerosol concentrations but also influence the physical properties of the ice. However, the localisation of impurities inside the microstructure is still under debate and little is known about the mineralogy of solid inclusions. In particular, the general mineralogical diversity throughout an ice core and the specific distribution inside the microstructure is poorly investigated; the impact of the mineralogy on the localisation of inclusions and other processes is thus hardly known. We use dust particle c

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49

Jones, Anthony P. "The mineralogy of cosmic dust: astromineralogy." European Journal of Mineralogy 19, no. 6 (2007): 771–82. http://dx.doi.org/10.1127/0935-1221/2007/0019-1766.

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50

Alcalde-Fuentes, María Rosario, Rosario García Giménez, Ramón Jiménez-Martínez, and Juan Alberto Pérez-Valera. "The Mineralogy Manuscript Preserved in the Archivo General de Palacio, (Madrid, Spain): A Case Study." Geosciences 15, no. 6 (2025): 196. https://doi.org/10.3390/geosciences15060196.

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The manuscript of the Mineralogical lessons for the 1824–1825 course being held at the Royal Cabinet of Natural History had been found in the Archivo General de Palacio (AGP; Madrid, Spain) by the priest Donato García, who replaced Christian Herrgen and held the chair of Mineralogy until 1853. The historic document increases the scant record of this type of documentary source from a period still little known in relation to the state of Mineralogy teaching and allows for a closer understanding of this discipline. This article presents a thorough analysis to identify the collaboration between Pr

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