Gotowe bibliografie tematyczne / Mineral magnetic

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Gotowa bibliografia na temat „Mineral magnetic”

Autor: Grafiati

Data publikacji: 6 września 2023

Data aktualizacji: 31 lipca 2025

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Artykuły w czasopismach na temat "Mineral magnetic"

Mulyana, Mulyana, Vistarani Arini Tiwow, and Sulistiawaty Sulistiawaty. "ANALISIS SUSEPTIBILITAS MAGNETIK TANAH TPA ANTANG MAKASSAR BERDASARKAN KEDALAMAN." ORBITA: Jurnal Kajian, Inovasi dan Aplikasi Pendidikan Fisika 8, no. 2 (2022): 234. http://dx.doi.org/10.31764/orbita.v8i2.11252.

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ABSTRAKAnalisis suseptibilitas magnetik pada tanah di TPA Antang Makassar berdasarkan kedalaman telah dilakukan. Studi ini bertujuan untuk menganalisis jenis mineral magnetik, domain magnetik, dan sumber mineral magnetik. Suseptibilitas magnetik diukur menggunakan alat Bartington MS2 Magnetic Susceptibility Meter dengan sensor MS2B yang bekerja pada dua frekuensi. Pengukuran suseptibilitas magnetik dilakukan dengan mengambil sampel pada lima titik dengan variasi kedalaman hingga 0-80 cm dari permukaan tanah. Hasil pengukuran menunjukkan bahwa nilai suseptibilitas magnetik di TPA Antang bervari

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Arifya, Eldiani, and Afdal Afdal. "Pemetaan Zona Potensi Emas Menggunakan Metode Geomagnet di Jorong Lubuak Sariak, Nagari Kajai, Pasaman Barat." Jurnal Fisika Unand 9, no. 4 (2021): 524–30. http://dx.doi.org/10.25077/jfu.9.4.524-530.2020.

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Penelitian untuk menentukan zona sebaran emas di Jorong Lubuak Sariak, Nagari Kajai, Kabupaten Pasaman Barat, Sumatra Barat telah dilakukan. Penelitian ini menggunakan metode magnetik pada daerah seluas 700 m2 dengan 70 titik. Hasil penelitian menunjukan emas berasosiasi dengan pirhotit dengan nilai suseptibilitas 0,00046-1,4 SI, pirit dengan suseptibilitas 0,000035-0,005 SI dan siderit dengan suseptibilitas magnetik 0,0013 – 0,011 SI yang merupakan mineral sulfida magnetik yang terdapat dalam batuan metamorf dan sedimen. Selain itu mineral emas juga beasosiasi dengan batuan beku intrusi yaitu

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-, Palkrisman, and Arif Budiman. "PEMETAAN PERSENTASE KANDUNGAN DAN NILAI SUSEPTIBILITAS MINERAL MAGNETIK PASIR BESI PANTAI SUNUR KABUPATEN PADANG PARIAMAN SUMATERA BARAT." Jurnal Fisika Unand 3, no. 4 (2024): 242–48. https://doi.org/10.25077/jfu.3.4.242-248.2014.

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ABSTRAKTelah dilakukan penelitian tentang pemetaan persentase kandungan dan nilai suseptibilitas mineral magnetik pasir besi Pantai Sunur Kabupaten Padang Â Pariaman menggunakan metode Anisotropy of Magnetic Susceptibility (AMS). Hasil perhitungan persentase kandungan mineral magnetik dari 55 sampel menunjukkan rentang nilai 6,5% hingga 61,3%. Hasil perhitungan suseptibilitas mineral magnetik dari 55 sampel menunjukkan rentang nilai 333,65 Ã— 10-8 m3/kg hingga 2883,67 Ã— 10-8 m3/kg, berdasarkan nilai ini dapat diperkirakan bahwa mineral utama penyusun pasir besi Pantai Sunur adalah hematit dan

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Tiwow, Vistarani Arini, Meytij Jeanne Rampe, Sulistiawaty Sulistiawaty, and Pariabti Palloan. "HUBUNGAN SUSEPTIBILITAS MAGNETIK DAN LOGAM BERAT PASIR BESI PANTAI SAMPULUNGAN, TAKALAR, SULAWESI SELATAN." ORBITA: Jurnal Pendidikan dan Ilmu Fisika 9, no. 2 (2023): 254. http://dx.doi.org/10.31764/orbita.v9i2.17326.

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ABSTRAKPantai Sampulungan merupakan salah satu pantai di Kabupaten Takalar, Sulawesi Selatan sebagai kawasan wisata. Aktivitas pengunjung di pantai ini dapat mempengaruhi kualitas pasir besi. Dengan demikian, perlu dilakukan investigasi sifat magnetik pasir besi dan hubungannya dengan logam berat. Studi ini bertujuan menganalisis sumber mineral magnetik serta hubungan suseptibilitas magnetik dan logam berat pasir besi Pantai Sampulungan. Pengukuran parameter magnetik seperti suseptibilitas magnetik menggunakan alat Bartington Susceptibility Meter dilengkapi sensor MS2B. Metode XRF digunakan un

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Boroallo, Anastacya, Vistarani Arini Tiwow, and Sulistiawaty Sulistiawaty. "STUDI MINERAL MAGNETIK TANAH TPA ANTANG MAKASSAR BERDASARKAN DATA SUSEPTIBILITAS MAGNETIK." ORBITA: Jurnal Kajian, Inovasi dan Aplikasi Pendidikan Fisika 9, no. 1 (2023): 16. http://dx.doi.org/10.31764/orbita.v9i1.11663.

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ABSTRAKTelah dilakukan penelitian untuk mengetahui nilai suseptibilitas magnetik pada tanah di TPA Antang Makassar berdasarkan sebaran. Suseptibilitas magnetik diukur menggunakanbartington MS2 Magnetic susceptibility meter dengan sensor MS2B yang bekerja pada dua frekuensi. Pengukuran suseptibilitas magnetik dilakukan dengan mengambil sampel pada 30 titik dengan jarak yang tidak ditentukan atau secara random. Hasil penelitian menunjukkan bahwa nilai suseptibilitas magnetik di TPA Antang Makassar bervariasi dengan rentang 1,442 m3/kg hingga 33,523 m3/kg dan suseptibilitas magnetik bergantung fr

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Didik, Lalu A., Isniwana Damayanti, Jumliati Jumliati, and Putri Dinda Alfadia Lestari. "Morphological Characteristics and Mineral Content Analysis of Magnetic Minerals Based on River and Coastal Sand using SEM-EDX." Jurnal Sains Dasar 10, no. 2 (2021): 44–50. http://dx.doi.org/10.21831/jsd.v10i2.42217.

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This study aims to analyze the mineral content and morphological characteristics of magnetic minerals based on coastal and river sand. Analysis of minerals content uses Atomic Absorption Spectroscopy (AAS) to determine the content of Fe and Energy Dispersive X-Ray (EDX) to determine the elements of magnetic minerals based on coastal and river sand. While the morphological characteristics were analyzed using Scanning Electron Microscope (SEM). Based on the AAS analysis, magnetic mineral based on coastal sand has higher Fe content (9.03 mg/gram) compared to magnetic mineral based on river sand (

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Tamuntuan, Gerald, Seni H. J. Tongkukut, and Guntur Pasau. "Analisis Suseptibilitas Dan Histeresis Magnetik Pada Endapan Pasir Besi Di Sulawesi Utara." Jurnal MIPA 6, no. 2 (2017): 105. http://dx.doi.org/10.35799/jm.6.2.2017.18008.

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Telah dilakukan pengukuran suseptibilitas dan hysteresis magnetic untuk mengetahui karakteristik magnetic endapan pasir besi pada beberapa lokasi di Sulawesi Utara. Lokasi pengambilan sampel dalam penelitian ini adalah tiga lokasi di pesisir timur semenanjung utara Pulau Sulawesi yaitu daerah Belang, Hais, dan Minanga, serta tiga lokasi di wilayah pesisir barat yaitu daerah Lalow, Inobonto, dan Lolan. Hasil yang diperoleh menunjukkan bahwa nilai suseptibilitas magnetic pada sampel-sampel pasir yang diukur bervariasi dari 7,73 × 10-8 m3kg-1 hingga 436,38 × 10-8 m3kg-1. Pengukuran suseptibilitas

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Hutabarat, Imelda, Maryono, Rudiyansah, Dikri Fajar Ramadan, and Koko Wigyantoro. "Indonesian Tungsten Mineralogy and Processing Concept." E3S Web of Conferences 543 (2024): 01005. http://dx.doi.org/10.1051/e3sconf/202454301005.

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Tungsten minerals which are major as Wolframite and Scheelite mineral are by-product minerals of Tin mineral known as Cassiterite. Tin minerals are mostly found in Bangka Island which is one of the islands in the Southeast Asian tin belt that makes Indonesia the largest Tin (Sn) producer in the world. This research aims to characterize the mineralogy of Tungsten and associated minerals for potential mineral processing to gain the Tungsten concentrates. The Tungsten minerals were collected from the eastern edge of Klabat Granite in Toboali District, South Bangka. The Tungsten minerals were magn

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Khuzaima, Nur, Khairel Rafezi, Nur Hidayah Ahmad Zaidi, M. K. R. Hashim, and Sheikh Abdul Rezan. "Minerals Characterization of Magnetic and Non-Magnetic Element from Black Sand Langkawi." Solid State Phenomena 280 (August 2018): 440–47. http://dx.doi.org/10.4028/www.scientific.net/ssp.280.440.

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Valuable minerals are defined as mineral which having good opportunities to economic and consireable important. The most commonly occurring sand mineral deposits are ilmenite, rutile, magnetite, cassiterite, monazite, tourmaline, zircon, kyanite, silimanite, and garnet. In Malaysia, mineral sand deposits is found in Langkawi which known as black sand Langkawi. Langkawi black sand having high amount of valuable minerals that is very crucial in the industrial and construction products. Characterizations of black sand acquire different techniques to concentrate and separate valuable minerals. The

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Wang, Weiwei, Erdou Li, Zhengyao Li, Weiyao Zhu, and Yuanyuan Wang. "Recovery of Xenotime and Florencite from Silicate Minerals Using a Combined Technique of Magnetic Separation and Flotation." Minerals 14, no. 11 (2024): 1073. http://dx.doi.org/10.3390/min14111073.

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Xenotime (YPO4), a significant phosphatic minerl rich in heavy rare earth elements (HREEs), typically associates with granitic rocks, exemplified in the Wolverine rare earth deposit in Australia. A mineral composition analysis indicates that the primary valuable minerals in the deposit are principally xenotime and minor florencite, with quartz and illite as the main gangue minerals, showing a relatively simple mineral composition. The grade of rare earth concentrate was increased to 14.29% and the recovery reached 94.48% through the magnetic separation pre-enrichment test. However, a high-grad

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Rozprawy doktorskie na temat "Mineral magnetic"

Yanmin, Wang. "Wet magnetic concentration for weakly magnetic mineral fines and ultrafines." Doctoral thesis, Luleå, 1993. http://urn.kb.se/resolve?urn=urn:nbn:se:ltu:diva-26710.

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The first objective of the thesis was to reveal the characteristic magnetic behaviour of natural weakly magnetic minerals (such as hematite and chromite), and the size limits of the particles recoverable by the existing modem high intensity and high gradient magnetic separators. The second objective was to enhance the particle aggregation andlor the magnetic response for wet magnetic concentration of the ultrafines which escaped from the separators. It was observed that weakly magnetic natural minerals (hematite and chromite) exhibited variations in the magnetic behaviour with respect to magne

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Schmidt, Volkmar. "Magnetic and mineral fabrics in carbonate rocks /." Zürich : ETH, 2007. http://e-collection.ethbib.ethz.ch/show?type=diss&nr=17090.

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Smith, J. P. "Mineral magnetic studies on two Shropshire-Cheshire meres." Thesis, University of Liverpool, 1985. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.372707.

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Watson, D. J. "Mineral magnetic and palaeomagnetic properties of continental shelf sediments." Thesis, University of Edinburgh, 1989. http://hdl.handle.net/1842/14648.

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Yang, Ying Ping. "Electromagnetic characteristics of synthetic rocks, and sulphide and oxide mineral assemblages." Thesis, The University of Sydney, 1995. https://hdl.handle.net/2123/26849.

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An understanding of the electromagnetic characteristics of sulphide-bearing and magnetite-bearing rock and ore samples is important in the interpretation of electromagnetic (EM) exploration data. In this research study of electromagnetic conductivity characteristics, a theoretical measurement basis was developed, synthetic analogue materials were studied and the theory and analogue results were related to rock samples of varied mineralogy, texture and mineral concentration. The theory developed for cylindrical core sample EM measurements agreed with experiments performed on standard conduct

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Sandström, Dan. "Solid state nuclear magnetic resonance studies of synthetic mineral surfaces." Doctoral thesis, Luleå tekniska universitet, Industriell miljö- och processteknik, 2006. http://urn.kb.se/resolve?urn=urn:nbn:se:ltu:diva-26480.

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Solid state 1H, 31P and 27Al Magic Angle Spinning (MAS) Nuclear Magnetic Resonance (NMR) was used in studies of surface species formed on a synthetic fluorapatite in aqueous suspensions at different pH with or without ions or ion complexes of iron or aluminium in the suspension. Different sites related to the PO43- ions at the mineral surface were suggested, POx, POxH and POxH2. Also, three sites formed of Ca2+, H+ and OH- ions at the fluorapatite surface CaOH2+, CaOH and Ca(OH) 2- were suggested. Both single-pulse and cross polarization MAS NMR experiments were used to measure the 1H, 31P and

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Sandström, Dan. "Solid state nuclear magnetic resonance studies of synthetic mineral surfaces /." Luleå : Luleå tekniska universitet/Tillämpad kemi och geovetenskap/Kemi, 2006. http://epubl.ltu.se/1402-1544/2006/26/LTU-DT-0626-SE.pdf.

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Hannam, Jacqueline Ann. "Processes and timescales of secondary magnetic mineral formation in topsoils." Thesis, University of Liverpool, 1999. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.366393.

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Yu, L. "Environmental applications of mineral magnetic measurement : Towards a quantitative approach." Thesis, University of Liverpool, 1989. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.234577.

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Jirestig, Jan A. "High intensity and high gradient magnetic separation in mineral processing." Doctoral thesis, Luleå tekniska universitet, 1994. http://urn.kb.se/resolve?urn=urn:nbn:se:ltu:diva-25815.

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Natural minerals often lack well defined magnetic susceptibilities. Instead they must be thought of as occurring in a susceptibility range where the bulk susceptibility is affected by present impurities. Inclusions or foreign atoms in solid solution may alter a materials magnetic properties to a large extent. Mixed particles of dia andlor paramagnetic materials display a linear relationship while ferromagnetic inclusions involve a demagnetisation factor. The susceptibility distribution of value minerals in relation to gangue in the ore is the most important factor governing magnetic separation

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Książki na temat "Mineral magnetic"

G, Andritzky, Geological Survey (Namibia), and Support to the Geological Survey/Mineral Prospecting Promotion (PN 90.2214.6) (Project : Namibia), eds. Integrated investigation of magnetic patterns in the Sinclair-Helmeringhausen area. Bundesanstalt für Geowissenschaften und Rohstoffe, 1996.

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G, Andritzky, Geological Survey (Namibia), and Support to the Geological Survey/Mineral Prospecting Promotion (PN 90.2214.6) (Project : Namibia), eds. Integrated investigation of magnetic patterns in and around the Rosh Pinah area. Bundesanstalt für Geowissenschaften und Rohstoffe, 1996.

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M, Wentzcovitch Renata, Navrotsky Alexandra, and Poeppelmeier Kenneth Reinhard, eds. Perovskite materials: Symposium held April 1-5, 2002, San Francisco, California, U.S.A. Materials Research Society, 2002.

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Booth, Colin Anthony. Sediment - source - linkages in the Gwendraeth Estuary, South Wales, based on mineral magnetic analyses. University of Wolverhampton, 2002.

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P, Frost Thomas, and Geological Survey (U.S.), eds. Analytical results of non-magnetic heavy-mineral-concentrate sample data from the Bethel and southern part of the Russian Mission 1p0s x 3p0s quadrangles, southwest Alaska. U.S. Dept. of the Interior, U.S. Geological Survey, 1993.

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Jones, Keith Richard. Circulation, deposition and post-depositional changes of sediment in two Welsh estuaries: A mineral magnetic investigation. University of Wolverhampton, 2001.

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Ford, Arthur B. Magnetic susceptibility and density determinations for plutonic and metamorphic rocks of the Glacier Peak Wilderness and vicinity, northern Cascades, Washington. Dept. of the Interior, U.S. Geological Survey, 1988.

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McMacken, David. The Saratoga of the West: The story of the Magnetic Mineral Spring and Park Hotel of St. Louis, Michigan. D. McMacken, 1986.

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Cikcik, Ali. Magnetic flocculation of weakly magnetic minerals. University of Birmingham, 1985.

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W, Day Gordon, and Geological Survey (U.S.), eds. Analytical results and sample locality map of nonmagnetic and moderately magnetic heavy-mineral concentrates from stream sediments from the Glens Falls 1. U.S. Dept. of the Interior, Geological Survey, 1986.

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Części książek na temat "Mineral magnetic"

Adeleke, Abraham Adewale. "Magnetic Separation." In Mineral Processing Technology. CRC Press, 2023. http://dx.doi.org/10.1201/9781003323433-14.

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Chelgani, Saeed Chehreh, and Ali Asimi Neisiani. "Magnetic Separation." In Dry Mineral Processing. Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-030-93750-8_2.

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Cohen, H. E. "Magnetic Separation." In Mineral Processing at a Crossroads. Springer Netherlands, 1986. http://dx.doi.org/10.1007/978-94-009-4476-3_10.

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Parker, M. R. "Processing of Mineral Ores by Modern Magnetic Separation Techniques." In Mineral Processing Design. Springer Netherlands, 1987. http://dx.doi.org/10.1007/978-94-009-3549-5_6.

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Thompson, Roy, and Frank Oldfield. "Mineral magnetic studies of lake sediments." In Environmental Magnetism. Springer Netherlands, 1986. http://dx.doi.org/10.1007/978-94-011-8036-8_10.

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Makarchuk, Oksana, Tetiana Dontsova, and Anatolii Perekos. "Magnetic Nanocomposite Sorbents on Mineral Base." In Springer Proceedings in Physics. Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-56422-7_54.

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Haas, T., Ph Jehenson, D. Hillion, et al. "Phosphate Transfer and 31P Nuclear Magnetic Resonance (NMR) Spectroscopy Pre and Post Hemofiltration (HF)." In Phosphate and Mineral Homeostasis. Springer US, 1986. http://dx.doi.org/10.1007/978-1-4684-5206-8_59.

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Shabanova, I. N., S. M. Reshetnikov, V. I. Kodolov, et al. "Investigation of Copper/Carbon Nanocomposites Modified with Phosphorus-Containing Groups as Inhibiting Additives in Mineral Oil." In Modern Magnetic Materials. Apple Academic Press, 2023. http://dx.doi.org/10.1201/9781003372066-5.

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Majumdar, Sharmila. "Magnetic Resonance Imaging of Bone." In Primer on the Metabolic Bone Diseases and Disorders of Mineral Metabolism. John Wiley & Sons, Inc., 2013. http://dx.doi.org/10.1002/9781118453926.ch32.

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McWhinnie, William R. "Electron Spin Resonance and Nuclear Magnetic Resonance Applied to Minerals." In Chemical Bonding and Spectroscopy in Mineral Chemistry. Springer Netherlands, 1985. http://dx.doi.org/10.1007/978-94-009-4838-9_6.

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Streszczenia konferencji na temat "Mineral magnetic"

Smothers, Kent W., Charles D. Curtiss, and Vincent F. Hock. "Demonstration and Evaluation of Magnetic Descalers." In CORROSION 2003. NACE International, 2003. https://doi.org/10.5006/c2003-03274.

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Abstract The formation of mineral scale in potable water heat exchangers and distribution piping reduces flow and system capacity, increases operational costs due impacts on efficiency, and can ultimately cause failure or result in the need for chemical cleaning. Chemical cleaning can be costly and could result in loss of service for an extended period. Additionally, chemically cleaning these types of systems poses a potential health risk to the building occupants. Traditional methods for preventing this problem from occurring include chemical treatment to soften the water, chemical inhibitors

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Marco, Surracco, and Tilocca Maria Caterina. "FLOTATION AND MAGNETIC SEPARATION PROCESSES FOR A MINERAL OF WOLLASTONITE." In 24th SGEM International Multidisciplinary Scientific GeoConference 24. STEF92 Technology, 2024. https://doi.org/10.5593/sgem2024/1.1/s04.56.

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This paper presents the results of laboratory processing tests conducted to explore the potential for beneficiation of a wollastonite mineral (calcium metasilicate, CaSiO3). The ore studied comes from a mineralized body located in the southern part of Sardinia (Italy), which has been studied in the past with geological surveys and sampling. In the investigated area the mineralization was very irregular. The encasing rocks consist of schist and the mineralized body is composed of wollastonite associated with limestone, garnets and silica. The sample used for treatment tests was taken from this

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Adebiyi, Leke Sunday, Sesan Cornelius Falade, Kehinde Oladele Dopamu, and Esther Adetola Alejolowo. "Mineral Potential of Parts of Southwestern Nigeria from Magnetic and Radiometric Methods." In 2024 International Conference on Science, Engineering and Business for Driving Sustainable Development Goals (SEB4SDG). IEEE, 2024. http://dx.doi.org/10.1109/seb4sdg60871.2024.10629717.

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Fitzgerald, D., R. Wackerle, and M. Morse. "Integrated 3D Modelling of Variable Magnetic Remanence Fields." In Mineral Exploration Symposium. European Association of Geoscientists & Engineers, 2020. http://dx.doi.org/10.3997/2214-4609.202089011.

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Yang, Zhengtao, Ali Shaito, and Nandika Anne D'Souza. "Magnetorheology of Multiwalled Carbon Nanotube Mineral Dispersions." In ASME 2006 International Mechanical Engineering Congress and Exposition. ASMEDC, 2006. http://dx.doi.org/10.1115/imece2006-16004.

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Multi-walled carbon nanotube (MWCNT) were dispersed in mineral oil and the magnetorheological response was measured. 0.5, 1.5 and 2.53 vol% nanotubes were dispersed in mineral oil. Strain sweep, frequency sweep, magneto sweep and steady shear tests were conducted in various magnetic field strengths. Storage modulus G', loss modulus G", complex viscosity η* and dynamic yield stress τy increased with magnetic field, which was partially attributed to the increasing degree of alignment of nanotubes in stronger magnetic field. G' and G" of MWCNT/mineral oil dispersions scaled with nanotube volume f

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Saylymby, Dayana Yu, Petr G. Dyadkov, and Nikolay Ed Mikhaltsov. "Curie temperature of the rocks of the Zarechenskay magnetic anomaly (East coast of Lake Baikal)." In Недропользование. Горное дело. Направления и технологии поиска, разведки и разработки месторождений полезных ископаемых. Экономика. Геоэкология. Федеральное государственное бюджетное учреждение науки Институт нефтегазовой геологии и геофизики им. А.А. Трофимука Сибирского отделения Российской академии наук, 2020. http://dx.doi.org/10.18303/b978-5-4262-0102-6-2020-064.

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The Curie temperature of rock samples of the Zarechenskaya magnetic anomaly region is determined. The source of this anomaly is an array of Archean rocks, composed mainly of gneiss–granits. The obtained values of the Curie temperature indicate that the magnetism of these rocks is due to magnetite. Both knowledge of the Curie temperature and the magnetic mineral responsible for the magnetism of this rock massive is important for interpreting the results of tectonomagnetic monitoring performed here since 1984, as well as for solving geothermal problems.

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Fitriani, Dini, Kartika Hajar Kirana, Eleonora Agustine, Mia Uswatun Hasanah, and dan Anggie Susilawati. "Magnetic susceptibility, morphological and magnetic mineral composition analysis on leachate sludge." In The 13th SEGJ International Symposium, Tokyo, Japan, 12-14 November 2018. Society of Exploration Geophysicists and Society of Exploration Geophysicists of Japan, 2019. http://dx.doi.org/10.1190/segj2018-116.1.

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Sankaya, M., M. Erdemoglu, and T. Abbasov. "Investigations on high gradient magnetic separation processes in rheological media." In The 8th International Mineral Processing Symposium. CRC Press, 2017. http://dx.doi.org/10.4324/9780203747117-24.

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Makarchuk, Oksana, Tetiana Dontsova, and Grigory Krymets. "Magnetic mineral nanocomposite sorbents for removal of surfactants." In 2017 IEEE 7th International Conference "Nanomaterials: Application & Properties" (NAP). IEEE, 2017. http://dx.doi.org/10.1109/nap.2017.8190406.

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Xu, Huifang, Seungyeol Lee, Hongwu Xu, Ryan Jacobs, and Dane Morgan. "VALLEYITE: A NEW MAGNETIC MINERAL IN BASALTIC ROCKS." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-297685.

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Raporty organizacyjne na temat "Mineral magnetic"

Hayward, N., and V. Tschirhart. A comparison of 3-D inversion strategies in the investigation of the 3-D density and magnetic susceptibility distribution in the Great Bear Magmatic Zone, Northwest Territories. Natural Resources Canada/CMSS/Information Management, 2023. http://dx.doi.org/10.4095/331954.

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The inversion of new compilations of aeromagnetic data and gravity data are employed to investigate the 3-D physical property (magnetic susceptibility and density) distribution within the Great Bear magmatic zone. The application of two different software suites (Geosoft VOXI and UBC GIF MAG3D and GRAV3D) affords a comparison of approaches and results. The magnetic susceptibility results are broadly compatible, but Geosoft VOXI enabled more detailed definition of shallow sources. The density results were markedly different in how the model responded to the low-resolution gravity data in charac

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Rheault, M. M., R. Simard, P. Keating, and M. M. Pelletier. Mineral exploration: digital image processing of LANDSAT, SPOT, magnetic and geochemical data. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1990. http://dx.doi.org/10.4095/128045.

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Hayward, N. 3D magnetic inversion of mineral prospects in the Great Bear Magmatic Zone, Northwest Territories. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2013. http://dx.doi.org/10.4095/292662.

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Thornell, Travis, Charles Weiss, Sarah Williams, et al. Magnetorheological composite materials (MRCMs) for instant and adaptable structural control. Engineer Research and Development Center (U.S.), 2020. http://dx.doi.org/10.21079/11681/38721.

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Magnetic responsive materials can be used in a variety of applications. For structural applications, the ability to create tunable moduli from relatively soft materials with applied electromagnetic stimuli can be advantageous for light-weight protection. This study investigated magnetorheological composite materials involving carbonyl iron particles (CIP) embedded into two different systems. The first material system was a model cementitious system of CIP and kaolinite clay dispersed in mineral oil. The magnetorheological behaviors were investigated by using parallel plates with an attached ma

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Bristow, Q., and C. J. Mwenifumbo. A new temperature, capacitive-resistivity, and magnetic-susceptibility borehole probe for mineral exploration, groundwater, and environmental applications. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2011. http://dx.doi.org/10.4095/289197.

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Thomas, M. D. Spatial relationship between porphyritic Cu-Au mineral occurrences and magnetic signatures within the Iron Mask Batholith, south-central Cordillera, British Columbia. Natural Resources Canada/CMSS/Information Management, 2021. http://dx.doi.org/10.4095/327943.

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Pisutha-Arnond, Visut, Sirichai Sunmanee, and Sudham Yaemniyom. A report on copper skarn deposit at Phu Lon, Amphoe Sang Khom Changwat Nong Khai. Chulalongkorn University, 1988. https://doi.org/10.58837/chula.res.1988.18.

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Based on the geological and petrographical studies and chemical analysis of drill-core and outcrop samples, the geology and mineralization at the Phu Lon area are revealed. The Phu Lon prospect is a Cu-Fe-Au-Ag skarn deposit of porphyry-related type. The copper- and iron-rich zones are hosted predominantly in the garnet-pyroxene skarn that is developed metasomatically at the contact between the diorite-monzodiorite intrusions and a marble with minor calcsilicate unit. The main stage of iron mineralization probably took place during the prograde garnet-pyroxene skarn formation and was genetical

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Mueller, C., S. J. Piercey, M. G. Babechuk, and D. Copeland. Stratigraphy and lithogeochemistry of the Goldenville horizon and associated rocks, Baie Verte Peninsula, Newfoundland. Natural Resources Canada/CMSS/Information Management, 2021. http://dx.doi.org/10.4095/328990.

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The Goldenville horizon in the Baie Verte Peninsula is an important stratigraphic horizon that hosts primary (Cambrian to Ordovician) exhalative magnetite and pyrite and was a chemical trap for younger (Silurian to Devonian) orogenic gold mineralization. The horizon is overlain by basaltic flows and volcaniclastic rocks, is intercalated with variably coloured argillites and cherts, and underlain by mafic volcaniclastic rocks; the entire stratigraphy is cut by younger fine-grained mafic dykes and coarser gabbro. Lithogeochemical signatures of the Goldenville horizon allow it to be divided into

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Magnetic data of magnetic mineral separates from core samples (200' - 823') from the U.S. Navy Simpson Core Test #18 well. Alaska Division of Geological & Geophysical Surveys, 1990. http://dx.doi.org/10.14509/18994.

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Maps showing distribution of anomalous concentrations of trace elements in the magnetic fraction of heavy-mineral concentrates, Domeland Wilderness and contiguous roadless areas, Kern and Tulare counties, California. US Geological Survey, 1985. http://dx.doi.org/10.3133/mf1395d.

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