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Journal articles on the topic 'Mineraloge'

Author: Grafiati

Published: 4 June 2021

Last updated: 12 February 2022

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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 (January 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 innehatte. Weiss entwickelte die Lehre Werners, die die Mineralogie einschließlich Geologie umfasste, in kristallographischer Hinsicht weiter, während sich später neben ihm zwei seiner Schüler anderen Teilgebieten der Mineralogie annahmen, G. Rose der speziellen Mineralogie und E. Beyrich der geologischen Paläontologie. Der Ausbau der Sammlungen durch eigene Aufsammlungen, Schenkungen und Käufe konnte in starkem Maße fortgesetzt werden, auch zunehmend in paläontologischer Hinsicht, sodass das Mineralogische Museum für das ganze Spektrum der Lehre gut bestückt war. Der streitbare Charakter von Weiss verursachte zahlreiche Reibungspunkte. <br><br> History of the Geoscience Institutes of the Natural History Museum in Berlin. Part 4 <br><br> The establishment of the University in Berlin in 1810 resulted in the adoption of the teaching of the dissolved Bergakademie and of the royal Mineralienkabinett of the Prussian mining department, which was used by the Bergakademie before it became the Mineralogical Museum of the University. The Bergakademie continued to exist only as Bergeleveninstitut or Bergelevenklasse for financing the education of the mining students. The physicist and mineralogist C. S. Weiss was offered the chair of mineralogy after the death of D. L. G. Karsten 1810; he had the position to his death in 1856. Weiss developped the crystallographic part of the science of Werner which included mineralogy and geology. Two of his pupils progressed two other parts of mineralogy, G. Rose the speciel mineralogy and E. Beyrich the geological paleontology. The enlargement of the collections continued on large scale by own collecting, donations and purchases, also more paleontological objects, so that the Mineralogical Museum presented a good collection of the whole spectrum of the field. The pugnacious nature of Weiss resulted in many points of friction. <br><br> doi:<a href="http://dx.doi.org/10.1002/mmng.20010040102" target="_blank">10.1002/mmng.20010040102</a>

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2

Hoppe, Günter. "Friedrich Tamnau (1802--1879) -- Mineraloge, Mineralsammler und Mäzen." Mitteilungen aus dem Museum für Naturkunde in Berlin. Geowissenschaftliche Reihe 7, no. 1 (October 10, 2004): 45–59. http://dx.doi.org/10.1002/mmng.4860070104.

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3

Hoppe, G. "Friedrich Tamnau (1802–1879) – Mineraloge, Mineralsammler und Mäzen." Fossil Record 7, no. 1 (January 1, 2004): 45–59. http://dx.doi.org/10.5194/fr-7-45-2004.

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Der Berliner Bankier Friedrich Tamnau betätigte sich neben seinem Beruf sein ganzes Leben lang als Mineraloge und mit großem finanziellem Aufwand als Mineralsammler. Seine berühmten Sammlungsbestände stellte er Fachleuten großzügig zur Verfügung. Eine erste große Sammlung verkaufte er 1841 der Berliner Universität. Seine noch größere zweite Sammlungsbeständte er am Lebensende testamentarisch der Berliner Technischen Hochschule. Außerdem gründete er die Tamnau-Stiftung, die der Finanzierung von Auslandsreisen zum Sammeln und Bearbeiten von Mineralen diente. <br><br> The banker Friedrich Tamnau, Berlin, was active as a mineralogist during his entire life while at the same time conducting his profession. He also a large financial imput into the collection of minerals. He generously offered his famous collection to scinetists for study. He sold his first large collection to the University of Berlin. A the end of his life he presented by testament a second even larger collection to the Technical University of Berlin. In addition he founded the Tamnau-Foundation to support foreign travel to collect and study minerals. <br><br> doi:<a href="http://dx.doi.org/10.1002/mmng.20040070104" target="_blank">10.1002/mmng.20040070104</a>

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Hoppe, G. "Zur Geschichte der Geowissenschaften im Museum für Naturkunde zu Berlin. Teil 3: Von A. G. Werner und R. J. Haüy zu C. S. Weiss – Der Weg von C. S. Weiss zum Direktor des Mineralogischen Museums der Berliner Universität." Fossil Record 3, no. 1 (January 1, 2000): 3–25. http://dx.doi.org/10.1002/mmng.20000030102.

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Abstract. Der Berufung von C. S. Weiss an die Universität Berlin im Jahre 1810 gingen Entwicklungen voraus, die durch die Kristallographie des Franzosen R. J. Haüy, besonders durch dessen Lehrbuch der Mineralogie, ausgelöst wurden. Sie stehen mit der Übersetzung dieses Lehrbuchs im Zusammenhang und führten zur Qualifizierung von C. S. Weiss zum Mineralogen und Kristallographen sowie zur weiteren Entwicklung der Kristallographie innerhalb des Lehrgebäudes der Mineralogie. Den Anstoß gab der mit dem Berliner Mineralogen D. L. G. Karsten befreundete Geologe L. v. Buch, der die Kristallographie Haüys als Erster kennen lernte. Als dessen stark kristallographisch orientiertes Lehrbuch der Mineralogie erschien, entschloss sich Karsten, eine kommentierte Übersetzung desselben zu organisieren. Weiss, der hierfür gewonnen werden konnte, bildete sich zunächst an der Bergakademie Freiberg weiter aus, wobei er die Lehre des führenden Mineralogen A. G. Werner voll in sich aufnahm. Im Verlaufe der Mitarbeit an der Übersetzung gelangte Weiss gegenüber den atomistischen Vorstellungen Haüys zu Ansichten über die Gesetzmäßigkeiten des Kristallbaues. die sich auf Kants Naturphilosophie gründeten. Mit Haüy, den er in Paris näher kennen lernte, kam es deshalb zum Bruch. Seine "dynamische" Kristallographie baute Weiss mathematisch aus und vermochte bereits weit in die Gesetzmäßigkeiten des Kristallbaues einzudringen. Dadurch schuf er die Voraussetzungen für seine Berufung auf den für Karsten vorgesehenen Berliner Mineralogie-Lehrstuhl, der durch dessen frühen Tod frei wurde. doi:10.1002/mmng.20000030102x

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5

Hoppe, G. "Zur Geschichte der Geowissenschaften im Museum für Naturkunde zu Berlin. Teil 3: Von A. G. Werner und R. J. Haüy zu C. S. Weiss – Der Weg von C. S. Weiss zum Direktor des Mineralogischen Museums der Berliner Universität." Fossil Record 3, no. 1 (January 1, 2000): 3–25. http://dx.doi.org/10.5194/fr-3-3-2000.

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Der Berufung von C. S. Weiss an die Universität Berlin im Jahre 1810 gingen Entwicklungen voraus, die durch die Kristallographie des Franzosen R. J. Haüy, besonders durch dessen Lehrbuch der Mineralogie, ausgelöst wurden. Sie stehen mit der Übersetzung dieses Lehrbuchs im Zusammenhang und führten zur Qualifizierung von C. S. Weiss zum Mineralogen und Kristallographen sowie zur weiteren Entwicklung der Kristallographie innerhalb des Lehrgebäudes der Mineralogie. Den Anstoß gab der mit dem Berliner Mineralogen D. L. G. Karsten befreundete Geologe L. v. Buch, der die Kristallographie Haüys als Erster kennen lernte. Als dessen stark kristallographisch orientiertes Lehrbuch der Mineralogie erschien, entschloss sich Karsten, eine kommentierte Übersetzung desselben zu organisieren. Weiss, der hierfür gewonnen werden konnte, bildete sich zunächst an der Bergakademie Freiberg weiter aus, wobei er die Lehre des führenden Mineralogen A. G. Werner voll in sich aufnahm. Im Verlaufe der Mitarbeit an der Übersetzung gelangte Weiss gegenüber den atomistischen Vorstellungen Haüys zu Ansichten über die Gesetzmäßigkeiten des Kristallbaues. die sich auf Kants Naturphilosophie gründeten. Mit Haüy, den er in Paris näher kennen lernte, kam es deshalb zum Bruch. Seine "dynamische" Kristallographie baute Weiss mathematisch aus und vermochte bereits weit in die Gesetzmäßigkeiten des Kristallbaues einzudringen. Dadurch schuf er die Voraussetzungen für seine Berufung auf den für Karsten vorgesehenen Berliner Mineralogie-Lehrstuhl, der durch dessen frühen Tod frei wurde. <br><br> doi:<a href="http://dx.doi.org/10.1002/mmng.20000030102" target="_blank">10.1002/mmng.20000030102x</a>

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6

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 (December 23, 2010): 897–908. http://dx.doi.org/10.1127/0935-1221/2010/0022-2047.

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7

Freedman, R., S. Herron, V. Anand, M. Herron, D. May, and D. Rose. "New Method for Determining Mineralogy and Matrix Properties From Elemental Chemistry Measured by Gamma Ray Spectroscopy Logging Tools." SPE Reservoir Evaluation & Engineering 18, no. 04 (November 25, 2015): 599–608. http://dx.doi.org/10.2118/170722-pa.

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Summary Methods for predicting mineralogy from logging-tool measurements have been an active area of research for several decades. In spite of these efforts, methods for predicting quantitative mineralogy including clay types from well-logging data were not fully achieved. The introduction of geochemical logging tools in the 1980s offered promise; however, early versions of geochemical logging tools did not measure elemental chemistry with enough accuracy and precision to enable reliable and quantitative determination of mineralogy. Recent advances in geochemical-logging-tool technology now enable accurate and robust measurements of the chemical elemental concentrations that are needed to determine continuous quantitative and detailed logs of mineralogy. This paper presents a novel approach for determining more accurate and more detailed mineralogy from an elemental spectroscopy logging tool. This work was made possible by three recent developments: the introduction of a new neutron-induced gamma ray spectroscopy logging tool, a new research database consisting of chemistry and mineralogy measured on cores acquired worldwide from conventional and unconventional reservoirs, and a new model-independent inversion method that overcomes the limitations of previous model-dependent methods. The model-independent inversion makes use of the database that includes clean sands, shaly sands, shales, carbonates, and complex mixed lithologies. The database contains laboratory measurements of dry-weight elemental chemistry and mineralogy measured by transmission Fourier-transform infrared (FTIR) spectroscopy. The database is used to derive a model-independent mapping function that accurately represents the complex functional relationship between the elemental concentrations and the mineral concentrations. After the mapping function is determined from the database, one can use it to predict quantitative mineralogy from elemental concentrations derived from the logging-tool measurements. Unlike previous inversion methods, the model-independent mapping function does not have any adjustable parameters or require any user inputs such as mineral properties or endpoints. The mapping function is used to predict continuous logs of matrix densities plus concentrations of 14 minerals (i.e., illite, smectite, kaolinite, chlorite, quartz, calcite, dolomite, ankerite, plagioclase, orthoclase, mica, pyrite, siderite, and anhydrite) from eight dry-weight elemental concentrations derived from the logging tool. The new method was applied to well-log data acquired worldwide in numerous conventional and unconventional reservoirs with a wide variety of complex mineralogies. The predicted mineralogies and matrix densities are generally found to be consistent with core-derived mineralogies and matrix densities.

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8

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 (January 3, 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 subject of the present work focuses in various lithotypes (monzodiorite, diorite, altered diorite, actinolite schist, cataclasite, slate) from Kos Island, Aegean Sea, in Greece, all bearing hydrous minerals in various amounts. The evaluation of the results obtained from NIR spectroscopy offered important qualitative information about the mineralogy of the lithotypes examined. The important asset of the method is that no sample preparation was necessary. From the reflectance spectra, the NIR-active minerals that were identified include chlorite, micas, amphiboles and epidotes. Petrographic and mineralogic analyses were also employed in order to confirm the NIR results and provide more detailed information about the mineralogy of the samples, the grain size and the orientation of the minerals. Correlation of wavelength positions at ~1400 nm with loss on ignition (LOI) values led us to relate the various lithotypes in terms of their petrological affinities. NIR spectroscopy was proved to be a useful tool, especially for the mineralogic identification of rocks underwent low- to medium grade metamorphism, from greenschist to amphibolite facies.

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Graham, Shaun, and Nynke Keulen. "Nanoscale Automated Quantitative Mineralogy: A 200-nm Quantitative Mineralogy Assessment of Fault Gouge Using Mineralogic." Minerals 9, no. 11 (October 29, 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 the Zeiss Mineralogic software platform, mixed signals could be deconvoluted down to a size of 200 nm. In this way, EDX and automated quantitative mineralogy can be applied to investigations of submicrometer-sized grains. It is shown here that reliable quantitative mineralogy and grain size distribution assessment can be made based on an example of fault gouge with a heterogenous mineralogy collected from Ikkattup nunaa Island, southern West Greenland.

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Casetou-Gustafson, Sophie, Cecilia Akselsson, Stephen Hillier, and Bengt A. Olsson. "The importance of mineral determinations to PROFILE base cation weathering release rates: a case study." Biogeosciences 16, no. 9 (May 7, 2019): 1903–20. http://dx.doi.org/10.5194/bg-16-1903-2019.

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Abstract. Accurate estimates of base cation weathering rates in forest soils are crucial for policy decisions on sustainable biomass harvest levels and for calculations of critical loads of acidity. The PROFILE model is one of the most frequently used methods to quantify weathering rates, where the quantitative mineralogical input has often been calculated by the A2M (“Analysis to Mineralogy”) program based solely on geochemical data. The aim of this study was to investigate how uncertainties in quantitative mineralogy, originating from modeled mineral abundance and assumed stoichiometry, influence PROFILE weathering estimate, by using measured quantitative mineralogy by X-ray powder diffraction (XRPD) as a reference. Weathering rates were determined for two sites, one in northern (Flakaliden) and one in southern (Asa) Sweden. At each site, 3–4 soil profiles were analyzed at 10 cm depth intervals. Normative quantitative mineralogy was calculated from geochemical data and qualitative mineral data with the A2M program using two sets of qualitative mineralogical data inputs to A2M: (1) a site-specific mineralogy based on information about mineral identification and mineral chemical composition as determined directly by XRPD and electron microprobe analysis (EMPA), and (2) regional mineralogy, representing the assumed minerals present and assumed mineral chemical compositions for large geographical areas in Sweden, as per previous published studies. Arithmetic means of the weathering rates determined from A2M inputs (WA2M) were generally in relatively close agreement with those (WXRPD) determined by inputs based on direct XRPD and EMPA measurements. The hypothesis that using site-specific instead of regional mineralogy will improve the confidence in mineral data input to PROFILE was supported for Flakaliden. However, at Asa, site-specific mineralogies reduced the discrepancy for Na between WA2M and WXRPD but produced larger and significant discrepancies for K, Ca and Mg. For Ca and Mg the differences between weathering rates based on different mineralogies could be explained by differences in the content of some specific Ca- and Mg-bearing minerals, in particular amphibole, apatite, pyroxene and illite. Improving the accuracy in the determination of these minerals would reduce weathering uncertainties. High uncertainties in mineralogy, due for example to different A2M assumptions, had surprisingly little effect on the predicted weathering of Na- and K-bearing minerals. This can be explained by the fact that the weathering rate constants for the minerals involved, e.g. K feldspar and micas, are similar in PROFILE. Improving the description of the dissolution rate kinetics of the plagioclase mineral group as well as major K-bearing minerals (K feldspars and micas) should be a priority to help improve future weathering estimates with the PROFILE model.

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Kohut, Connie K., and M. J. Dudas. "Evaporite mineralogy and trace-element content of salt-affected soils in Alberta." Canadian Journal of Soil Science 73, no. 4 (November 1, 1993): 399–409. http://dx.doi.org/10.4141/cjss93-042.

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A survey of efflorescent crusts and associated surface soils in central and southern Alberta was conducted to determine evaporite mineralogy and elemental composition. X-ray powder diffraction indicates that efflorescence mineralogies are dominated by sodium sulfate minerals, such as thenardite and mirabilite. Sodium magnesium sulfate minerals such as konyaite and bloedite are also frequently present, with eugsterite, halite and thermonatrite among other evaporites identified. The content of selected elements in the salt crusts and surface soils was determined using instrumental neutron activation analysis. Trace-element concentrations from site to site were extremely variable. However, comparisons with elemental abundances previously reported for till and soils indicate that there is generally no mean accumulation of trace elements in salt-affected soils. Exceptions are Br and Cl, which show enrichment in soils infused with soluble salts. Key words: Salinity, trace elements, evaporites, mineralogy

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Scanza, R. A., N. Mahowald, S. Ghan, C. S. Zender, J. F. Kok, X. Liu, and Y. Zhang. "Modeling dust as component minerals in the Community Atmosphere Model: development of framework and impact on radiative forcing." Atmospheric Chemistry and Physics Discussions 14, no. 12 (July 2, 2014): 17749–816. http://dx.doi.org/10.5194/acpd-14-17749-2014.

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Abstract. The mineralogy of desert dust is important due to its effect on radiation, clouds and biogeochemical cycling of trace nutrients. This study presents the simulation of dust radiative forcing as a function of both mineral composition and size at the global scale using mineral soil maps for estimating emissions. Externally mixed mineral aerosols in the bulk aerosol module in the Community Atmosphere Model version 4 (CAM4) and internally mixed mineral aerosols in the modal aerosol module in the Community Atmosphere Model version 5.1 (CAM5) embedded in the Community Earth System Model version 1.0.5 (CESM) are speciated into common mineral components in place of total dust. The simulations with mineralogy are compared to available observations of mineral atmospheric distribution and deposition along with observations of clear-sky radiative forcing efficiency. Based on these simulations, we estimate the all-sky direct radiative forcing at the top of the atmosphere as +0.05 W m−2 for both CAM4 and CAM5 simulations with mineralogy and compare this both with simulations of dust in release versions of CAM4 and CAM5 (+0.08 and +0.17 W m−2) and of dust with optimized optical properties, wet scavenging and particle size distribution in CAM4 and CAM5, −0.05 and −0.17 W m−2, respectively. The ability to correctly include the mineralogy of dust in climate models is hindered by its spatial and temporal variability as well as insufficient global in-situ observations, incomplete and uncertain source mineralogies and the uncertainties associated with data retrieved from remote sensing methods.

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Scanza, R. A., N. Mahowald, S. Ghan, C. S. Zender, J. F. Kok, X. Liu, Y. Zhang, and S. Albani. "Modeling dust as component minerals in the Community Atmosphere Model: development of framework and impact on radiative forcing." Atmospheric Chemistry and Physics 15, no. 1 (January 15, 2015): 537–61. http://dx.doi.org/10.5194/acp-15-537-2015.

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Abstract. The mineralogy of desert dust is important due to its effect on radiation, clouds and biogeochemical cycling of trace nutrients. This study presents the simulation of dust radiative forcing as a function of both mineral composition and size at the global scale, using mineral soil maps for estimating emissions. Externally mixed mineral aerosols in the bulk aerosol module in the Community Atmosphere Model version 4 (CAM4) and internally mixed mineral aerosols in the modal aerosol module in the Community Atmosphere Model version 5.1 (CAM5) embedded in the Community Earth System Model version 1.0.5 (CESM) are speciated into common mineral components in place of total dust. The simulations with mineralogy are compared to available observations of mineral atmospheric distribution and deposition along with observations of clear-sky radiative forcing efficiency. Based on these simulations, we estimate the all-sky direct radiative forcing at the top of the atmosphere as + 0.05 Wm−2 for both CAM4 and CAM5 simulations with mineralogy. We compare this to the radiative forcing from simulations of dust in release versions of CAM4 and CAM5 (+0.08 and +0.17 Wm−2) and of dust with optimized optical properties, wet scavenging and particle size distribution in CAM4 and CAM5, −0.05 and −0.17 Wm−2, respectively. The ability to correctly include the mineralogy of dust in climate models is hindered by its spatial and temporal variability as well as insufficient global in situ observations, incomplete and uncertain source mineralogies and the uncertainties associated with data retrieved from remote sensing methods.

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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 quick, cost-efficient, and nondestructive technique for analyzing soil mineralogic properties of large datasets. The main objectives of this review are to bring readers up to date with information and understanding of VNIR as it relates to soil mineralogy and attracts more attention from a wide variety of readers to revisit soil mineralogy. We begin our review with a description of fundamentals of VNIR. We then review common methods to process soil VNIR spectra and summary spectral features of soil minerals with particular attention to those <2 μm fractions. We further critically review applications of chemometric methods and related model building in spectroscopic soil mineral studies. We then compare spectral measurement with multivariate calibration methods, and we suggest that they both produce excellent results depending on the situation. Finally, we suggest a few avenues of future research, including the development of theoretical calibrations of VNIR more suitable for various soil samples worldwide, better elucidation of clay mineral-soil organic carbon (SOC) interactions, and building the concept of integrated soil mapping through combined information (e.g., mineral composition, soil organic matter-SOM, SOC, pH, and moisture).

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Naldrett, A. J. "Mineralogy is alive." European Journal of Mineralogy 12, no. 1 (February 7, 2000): 5–6. http://dx.doi.org/10.1127/ejm/12/1/0005.

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Neves, Paulo Cesar Pereira das, Percio de Moraes Branco, and Paulo Anselmo Matioli. "THE PERCIO DE MORAES BRANCO COLLECTION OF RARE MINERALS OF THE UNIVERSIDADE LUTERANA DO BRASIL (ULBRA)." SOUTHERN BRAZILIAN JOURNAL OF CHEMISTRY 5, no. 5 (December 20, 1997): 51–66. http://dx.doi.org/10.48141/sbjchem.v5.n5.1997.52_1997.pdf.

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The Mineral Collection of the Lutheran University of Brazil is one of the most valuable mineral collections of the South American Continent and consists of approximately 500 cataloged minerals, of which about 200 can be classified as rare or very rare. The majority of them are present in paragenesis with other minerals in the form of euhedric, subhedric, and anhedric crystals. The minerals come from different mineralogic provinces, including Denmark, the United States of America, Canada, Italy, Romania, Russia, Sweden, Brazil, Mexico, Chile, Slovenia, Germany, Algeria, England, and others. The Collection is organized in mineralogical classes with the exception of meteorites, organic compounds, and mineraloids and is found on permanent display and open to visitors in the Laboratory of Mineralogy, Building I, Central Campus of ULBRA in Canoas, RS, Brazil.

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van Hullebusch, Eric, and Stephanie Rossano. "Mineralogy, environment and health." European Journal of Mineralogy 22, no. 5 (November 2, 2010): 627. http://dx.doi.org/10.1127/0935-1221/2010/0022-2064.

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18

Dantas-Silva, Ana Beatriz, and Carlos Roberto Candeiro. "Relato de Experiência: Atividade de Monitoria em Mineralogia Aplicada à Química no Campus Pontal da Universidade Federal de Uberlândia." UNICIÊNCIAS 22, no. 1 (September 6, 2018): 33. http://dx.doi.org/10.17921/1415-5141.2018v22n1p33-37.

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A disciplina de Mineralogia está presente no programa curricular do curso de graduação em Química Bacharelado na Faculdade de Ciências Integradas do Pontal, Universidade Federal de Uberlândia. No início da disciplina, nota-se que há dificuldade no aprendizado dos alunos, entretanto, com o auxílio da atividade de monitoria e atividades didáticas, os alunos passam a compreender melhor o que está sendo abordado em sala de aula. Nesse intuito, o aluno monitor, com o objetivo de contribuir para a formação acadêmica dos estudantes, começa a desenvolver um perfil acadêmico melhorando o ensino-aprendizado de ambas as partes. Para isso, o trabalho foi dividido em várias etapas durante o semestre como: “levantamento bibliográfico, elaboração de questões, correção de provas, participação nas apresentações de filmes e trabalho de campo e auxílio na construção da caixa didática”. Desta maneira, a atividade de monitoria alcançou seu objetivo que é proporcionar ao discente uma visão geral do conhecimento abordado, além de contribuir para a formação acadêmica do aluno monitor.Palavras-chave: Mineralogia. Química. Monitoria. Ensino Aprendizado.AbstractThe discipline of Mineralogy is present in the curricular program of the undergraduation course in Chemistry at the Faculdade de Ciências Integradas do Pontal, Universidade Federal de Uberlândia. In the beginning of the discipline, it is noted that there is difficulty in the learning of the students, however, with the help of the activity of monitoring and didactic activities, the students come to better understand what is being addressed in the classroom. In this sense, the student monitor, with the aim of contributing to the academic training of students, begins to develop an academic profile improving the teaching-learning of both parties. For this, the work was divided into several stages during the semester such as: "bibliographic survey, elaboration of questions, correction of tests, participation in the presentations of films and field work and help in the construction of the didactic box". In this way, the monitoring activity reached its objective, which is to provide the student with a general vision of the knowledge addressed, in addition to contributing to the academic training of the student monitor.Keywords: Mineralogy. Chemistry. Monitoring. Teaching Learning.

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Keulen, Nynke, Sebastian Næsby Malkki, and Shaun Graham. "Automated Quantitative Mineralogy Applied to Metamorphic Rocks." Minerals 10, no. 1 (January 3, 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 to create mineral maps, element concentration maps, element ratio maps, mineral association maps, as well as to morphochemically classify individual minerals for their grain shape, size, and orientation. The visualization of metamorphic textures, while at the same time quantifying their textures, is the great strength of AQM and is an ideal tool to lift microscopy from the qualitative to the quantitative level.

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Hoppe, G. "Zur Geschichte der Geowissenschaften im Museum für Naturkunde zu Berlin. Teil 5: Vom Mineralogischen Museum im Hauptgebäude der Universität zu den zwei geowissenschaftlichen Institutionen im Museum für Naturkunde – 1856 bis 1910." Fossil Record 6, no. 1 (January 1, 2003): 3–51. http://dx.doi.org/10.5194/fr-6-3-2003.

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Im vorhergehenden 4. Teil der Artikelserie wurde die Zeit behandelt, in der das Gesamtgebiet der Geowissenschaften von dem Mineralogen und Kristallographen Christian Samuel Weiss im Mineralogischen Museum vertreten wurde und in der sich die Spezialisierung in Teilgebiete durch auftretende weitere Lehrkräfte zeigte. Nach dem Tod von Weiss im Jahre 1856 wirkte sich diese Entwicklung auch auf die Leitung des Mineralogischen Museums aus und führte schließlich zur Teilung in zwei Institutionen. Der vorliegende Artikel, der bis zum 100jährigen Jubiläum der Universität im Jahre 1910 reicht, behandelt dies in folgenden Kapiteln: 1) das Mineralogische Museum unter dem Mineralogen Gustav Rose als Direktor und dem Geologen und Paläontologen Ernst Beyrich in der Zeit von 1856 bis 1873, 2) das Mineralogische Museum unter Ernst Beyrich als Direktor, dem Mineralogen Martin Websky und dem Geologen und Petrographen Justus Roth in den Jahren von 1873 bis 1888 nebst Aufteilung in zwei Institutionen, 3) die Projektierung und den Bau des Museums für Naturkunde in den Jahren von 1873 bis 1889, 4) die beiden geowissenschaftlichen Institutionen in den Jahren 1888 bis 1910, 4a) das Geologisch-Paläontologische Institut und Museum unter den Geologen und Paläontologen Ernst Beyrich, Wilhelm Dames und Wilhelm Branco (Branca) nacheinander als Direktoren und 4b) das Mineralogisch-Petrographische Institut und Museum unter dem Mineralogen und Petrographen Carl Klein und danach dem Mineralogen und Kristallographen Theodor Liebisch als Direktoren. <br><br> The preceding fourth part of this series of articles dealt with the period (of time), when the whole field of earth sciences in the Mineralogical Museum was represented by one person, the mineralogist and crystallographer Christian Samuel Weiss. At that time the specialisation of earth sciences into different fields was already becoming evident from the practices of other academic teachers. After Weiss died in 1856, this process influenced the direction of the Museum of Mineralogy in such a way that it was divided into two institutions. This article covers the interval up to the Humboldt University's 100th anniversary in 1910. It is structured as follows: 1) The Mineralogical Museum under the directorship of the mineralogist Gustav Rose and the palaeontologist Ernst Beyrich from 1856 until 1873; 2) the Mineralogical Museum under the directorship of Ernst Beyrich, the mineralogist Martin Websky and the geologist and petrographer Justus Roth from 1873 to 1889, and its division into two institutions; 3) the planning and construction of the Museum für Naturkunde from 1873 to 1889; 4) the two geoscientific institutions from 1888 to 1910; 4a) the Geological-Palaeontological Institute and Museum under the successive directorships of the geologists and palaeontologists Ernst Beyrich, Wilhelm Beyrich, E. Dames and Wilhelm Branco (Branca); 4b) the Mineralogical-Petrographical Institute under the directorship of the mineralogist and petrographer Carl Klein and afterwards under the directorship of the mineralogist and petrographer Theodor Liebisch. <br><br> doi:<a href="http://dx.doi.org/10.1002/mmng.20030060102" target="_blank">10.1002/mmng.20030060102</a>

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21

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

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22

Artioli, Gilberto, and Ivana Angelini. "Mineralogy and archaeometry: fatal attraction." European Journal of Mineralogy 23, no. 6 (December 21, 2011): 849–55. http://dx.doi.org/10.1127/0935-1221/2011/0023-2119.

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23

Passaglia, Elio, and Ermanno Galli. "Natural zeolites: mineralogy and applications." European Journal of Mineralogy 3, no. 4 (August 27, 1991): 637–40. http://dx.doi.org/10.1127/ejm/3/4/0637.

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Clemens, Karen E., and Paul D. Komar. "TRACERS OF SAND MOVEMENT ON THE OREGON COAST." Coastal Engineering Proceedings 1, no. 21 (January 29, 1988): 100. http://dx.doi.org/10.9753/icce.v21.100.

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The study of sand mineralogy and grain rounding can help answer many questions of immediate concern to coastal engineers or to broader issues of beach preservation. The heavy-mineral contents of sands, together with statistical techniques such as factor analysis, can be used to delineate sediment sources, trace transport paths, and map out patterns of mixing during sediment dispersal. Variations in the degree of grain rounding can similarly be used to trace sand movements, or to obtain additional information concerning the history of the sediment particles. The techniques of studying sand mineralogies and grain rounding, and the types of problems they can address, are illustrated by research on the Oregon coast. Heavy mineral compositions of Oregon beach sands are the products of mixing contributions from four sources; the Columbia River on the north, the smaller rivers draining the Coast Range, the Umpqua River on the southern Oregon coast, and the Klamath Mountains of southern Oregon and northern California. Numerous headlands now prevent the longshore transport and mixing of sands from these multiple sources. The beach-sand compositions instead reflect along-coast mixing during Pleistocene lowered sea levels when blockage by headlands was absent. At that time there was a net littoral sand transport to the north, evident from the dispersal of Klamath-derived sands. With a rise in sea level and accompanying migrations of the beaches, headlands eventually interrupted the along-coast mixing of nearshore sands. Therefore, the north to south variation in compositions of beach sands is in part a relict pattern inherited from mixing during lowered sea levels. This has been modified during the past several thousand years by some additions of sand to the beaches from sea-cliff erosion and from rivers. However, studies of sediment mineralogy and grain rounding indicate that sands derived from most rivers draining the Coast Range are presently trapped in estuaries and so are not significant sources of beach sand. The Columbia River now supplies sand to Oregon beaches only to the first headland, Tillamook Head. At that headland there is a marked change in mineralogy and grain rounding with angular, recently supplied Columbia River sand to the north and rounded relict sand to the south.

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Shaw, R., L. Brebber, C. Ahern, and M. Weinand. "A review of sodicity and sodic soil behavior in Queensland." Soil Research 32, no. 2 (1994): 143. http://dx.doi.org/10.1071/sr9940143.

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The occurrence of sodic soils in Queensland is more related to soil genetic factors of the past than to the current rainfall pattern, with lower sodium accessions and smaller occurrence of saline lands than other areas of Australia. A soil sodicity map of Queensland is presented. On an area basis, 55% of soils in Queensland are non-sodic, 25% are strongly sodic and 20% are of variable sodicity. The map was prepared using exchangeable sodium percentage (ESP) values at 0.6 m depth from 2 009 soil profiles, as well as the soil boundaries of the 1:2000000 Atlas of Australian Soils maps (Northcote et al. 1960-68). There is general agreement with the earlier sodicity map of Northcote and Skene (1972). The relationships between exchangeable sodium and field-measured soil hydraulic properties and plant-available water capacity are discussed. Behaviour of sodic soils depends on the exchangeable sodium percentage, clay content, clay mineralogy and salt levels. The binary component particle packing theory has been used to explain soil behaviour and identify those soils most susceptible to sodium. Cracking clay soils with dominantly smectite mineralogy and high clay contents are less susceptible to a given ESP level, as determined by their hydrological behaviour, than soils of moderate clay content and mixed mineralogies. The sodicity and the salt content of an irrigation water are important in maintaining permeability of soils. The naturally occurring equilibrium salinity-sodicity relationships of a wide range of subsoils in Queensland is compared to the published relationships between stable permeability and decreasing permeability based on sodicity and salt content. Aspects of management of sodicity under dryland and irrigation are discussed.

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26

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

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27

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 (December 1, 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 techniques were tested using a data set of multielement geochemistry and mineralogy measured by semiquantitative X-ray diffraction data from the Productora Cu-Au-Mo deposit, Chile. Using geochemistry, samples from Productora were classified into populations based on their dominant alteration assemblage, including quartz-rich, Fe oxide, sodic, potassic, muscovite (sericite)- and clay-alteration, and least altered populations. Samples were also classified by their dominant sulfide mineralogy. Results indicate that alteration mapping through a range of graphical plots provides a rapid and simple appraisal of dominant mineral assemblage, which closely matches the measured mineralogy. In this study, calculated mineralogy using linear programming was also used to generate robust quantitative estimates for major mineral phases, including quartz and total feldspars as well as pyrite, iron oxides, chalcopyrite, and molybdenite, which matched the measured mineralogy data extremely well (R2 values greater than 0.78, low to moderate root mean square error). The results demonstrate that calculated mineralogy can be applied in the mining environment to significantly increase bulk mineralogy data and quantitatively map mineralogical variability. This was useful even though several minerals were challenging to model due to compositional similarities and clays and carbonates could not be predicted accurately.

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Thewalt, Ulf, and Gerda Dörfner. "Contributions to the mineralogy of the area of Ulm, Southern Germany." Jahresberichte und Mitteilungen des Oberrheinischen Geologischen Vereins 93 (April 26, 2011): 149–97. http://dx.doi.org/10.1127/jmogv/93/2011/149.

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29

Jones, Anthony P. "The mineralogy of cosmic dust: astromineralogy." European Journal of Mineralogy 19, no. 6 (December 17, 2007): 771–82. http://dx.doi.org/10.1127/0935-1221/2007/0019-1766.

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30

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 the beginning of 1983. The main directions of the development of technological mineralogy and the role of the published works of the commission are substantiated.

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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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32

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

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

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34

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

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35

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

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36

Kenter, Jeroen A. M., F. F. Podladchikov, Marc Reinders, Sjierk J. Van der Gaast, Bruce W. Fouke, and Mark D. Sonnenfeld. "Parameters controlling sonic velocities in a mixed carbonate‐siliciclastics Permian shelf‐margin (upper San Andres formation, Last Chance Canyon, New Mexico)." GEOPHYSICS 62, no. 2 (March 1997): 505–20. http://dx.doi.org/10.1190/1.1444161.

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We have measured the acoustic properties and mineralogic composition of 48 rock specimens from mixed carbonate‐siliciclastic outcrops of the Permian upper San Andres formation in Last Chance Canyon, New Mexico. The goals were: (1) identify and model the parameters controlling the sonic velocities; (2) assess the influence of postburial diagenesis on the acoustic velocities. The variation in sonic velocity in the 0 to 25% porosity range is primarily controlled by porosity, and secondly by the ratio of carbonate‐siliciclastic material. Linear multivariate fitting resulted in a velocity‐porosity‐carbonate content transform that accurately predicts sonic velocity at different effective stresses. The slope of the velocity‐porosity transform steepens with increasing carbonate content, which may be explained by the higher velocity of carbonate minerals. Another reason may be the property of carbonate minerals to form more perfect intercrystalline boundaries that improve the transmission properties of acoustic waves and are less sensitive to changes in effective stress. The velocity ratio [Formula: see text] is an excellent tool to discriminate between predominantly calcitic lithologies (ratio between 1.8 and 1.95) and predominantly dolomitic and quartz‐rich lithologies (ratio between 1.65 and 1.8). Gardner's experimental curve overestimates, and the velocity‐porosity transforms by Wyllie and Raymer underestimate, the observed sonic velocities, probably because they do not account for variations in texture, carbonate mineralogy, and pore geometry. Petrographic observations show that postburial diagenesis is minor and does not seem to significanfly affect porosity. Therefore, the outcrop data set can be regarded as a proxy for the subsurface analog. These findings underline the significantly more complex acoustic behavior in mixed carbonate‐siliciclastic sedimentary rocks than in pure siliciclastics where mineralogic composition explains most of the observed relationships between porosity and sonic velocity.

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Halley, Scott. "Mapping Magmatic and Hydrothermal Processes from Routine Exploration Geochemical Analyses." Economic Geology 115, no. 3 (May 1, 2020): 489–503. http://dx.doi.org/10.5382/econgeo.4722.

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Abstract Analytical methods used by commercial assay laboratories have improved enormously in recent years. Inductively coupled plasma-atomic emission spectroscopy and inductively coupled plasma-mass spectrometry methods now report analyses for half of the periodic table with exceptional detection limits and precision. It is becoming commonplace for mining companies to use such methods routinely for the analysis of drill samples throughout mineral deposits. Improvements in software and computing power now allow rapid interrogation of upward of 100,000 assay samples. Geochemical analyses are quantitative, are independent of observer bias, and can form the basis for robust geologic and mineralogical models of mineral deposits, as well as shed light on scientific questions. In particular, consistently collected, high-quality geochemical analyses can significantly improve and systematize logging of lithological and hydrothermal alteration mineralogic changes within drill core. In addition, abundant, high-quality geochemical data provide insights into magmatic and hydrothermal processes that were previously difficult to recognize and that have obvious applications to mineral exploration and improved genetic models of ore deposits. This paper describes a workflow that mining industry geologists can apply to their multielement analysis data to extract more information about magma compositions and gangue mineralogy.

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Yvon, Jacques, Philippe Marion, Laurent Michot, Frédéric Villieras, Friedrich Ernst Wagner, and Jοspeh Friedl. "Development of mineralogy applications in mineral processing." European Journal of Mineralogy 3, no. 4 (August 27, 1991): 667–76. http://dx.doi.org/10.1127/ejm/3/4/0667.

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Schneer, Cecil J. "Origins of mineralogy: the age of Agricola." European Journal of Mineralogy 7, no. 4 (August 1, 1995): 721–34. http://dx.doi.org/10.1127/ejm/7/4/0721.

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40

Rundqvist, D. V. "Mineralogy of large and superlarge mineral deposits." Global Tectonics and Metallogeny 9 (January 1, 2007): 3–12. http://dx.doi.org/10.1127/gtm/9/2007/3.

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41

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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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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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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44

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

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Bautsch, H. J. "Mineralogie. 3. Auflage." Zeitschrift für Kristallographie 194, no. 1-2 (January 1991): 156–57. http://dx.doi.org/10.1524/zkri.1991.194.1-2.156.

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47

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

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48

Vaughan, David J., and Claire L. Corkhill. "Mineralogy of Sulfides." Elements 13, no. 2 (April 1, 2017): 81–87. http://dx.doi.org/10.2113/gselements.13.2.81.

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49

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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50

Haditsch, J. G. "Grundwissen in Mineralogie." TMPM Tschermaks Mineralogische und Petrographische Mitteilungen 34, no. 3-4 (1985): 311–15. http://dx.doi.org/10.1007/bf01082970.

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