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Статті в журналах з теми "Melt source"
Maaløe, S. "Melt dynamics of a layered mantle plume source." Contributions to Mineralogy and Petrology 133, no. 1-2 (October 1998): 83–95. http://dx.doi.org/10.1007/s004100050439.
Повний текст джерелаMoallemi, M. K., and R. Viskanta. "Melting Around a Migrating Heat Source." Journal of Heat Transfer 107, no. 2 (May 1, 1985): 451–58. http://dx.doi.org/10.1115/1.3247436.
Повний текст джерелаSearle, M. P., J. M. Cottle, M. J. Streule, and D. J. Waters. "Crustal melt granites and migmatites along the Himalaya: melt source, segregation, transport and granite emplacement mechanisms." Earth and Environmental Science Transactions of the Royal Society of Edinburgh 100, no. 1-2 (March 2009): 219–33. http://dx.doi.org/10.1017/s175569100901617x.
Повний текст джерелаGuo, Kai, Yunping Ji, Yiming Li, Xueliang Kang, Huiyi Bai, and Huiping Ren. "Numerical Simulation of Temperature Field and Melt Pool Characteristics of CP-Ti Manufactured by Laser Powder Bed Fusion." Metals 13, no. 1 (December 20, 2022): 11. http://dx.doi.org/10.3390/met13010011.
Повний текст джерелаKnapp, J. A., L. R. Thompson, and G. J. Collins. "The role of radiation in melt stability in zone-melt recrystallization of SOI." Journal of Materials Research 5, no. 5 (May 1990): 998–1002. http://dx.doi.org/10.1557/jmr.1990.0998.
Повний текст джерелаWieser, Penny, Maurizio Petrelli, Jordan Lubbers, Eric Wieser, Sinan Ozaydin, Adam Kent, and Christy Till. "Thermobar: An open-source Python3 tool for thermobarometry and hygrometry." Volcanica 5, no. 2 (November 9, 2022): 349–84. http://dx.doi.org/10.30909/vol.05.02.349384.
Повний текст джерелаMaaløe, S. "Extraction of melt from veined mantle source regions during eruptions." Journal of Volcanology and Geothermal Research 147, no. 3-4 (October 2005): 377–90. http://dx.doi.org/10.1016/j.jvolgeores.2005.04.016.
Повний текст джерелаDiener, Johann F. A., Richard W. White, and Timothy J. M. Hudson. "Melt production, redistribution and accumulation in mid-crustal source rocks, with implications for crustal-scale melt transfer." Lithos 200-201 (July 2014): 212–25. http://dx.doi.org/10.1016/j.lithos.2014.04.021.
Повний текст джерелаKirdyashkin, A. A., A. G. Kirdyashkin, V. E. Distanov, and I. N. Gladkov. "ON HEAT SOURCE IN SUBDUCTION ZONE." Geodynamics & Tectonophysics 12, no. 3 (September 17, 2021): 471–84. http://dx.doi.org/10.5800/gt-2021-12-3-0534.
Повний текст джерелаAyoola, W. A., W. J. Suder, and S. W. Williams. "Comparison of Theoretical Disc and Point Source Profiles with Actual-Melt Source Profile in Conduction Welding." Nigerian Journal of Technological Development 19, no. 3 (September 23, 2022): 260–65. http://dx.doi.org/10.4314/njtd.v19i3.8.
Повний текст джерелаДисертації з теми "Melt source"
Gomez-Ulla, Rubira Alejandra. "Historical eruptions of Lanzarote, Canary Islands : Inference of magma source and melt generation from olivine and its melt inclusions." Thesis, Université Clermont Auvergne (2017-2020), 2018. http://www.theses.fr/2018CLFAC023.
Повний текст джерелаThe study of oceanic island basalts (OIB) reveals the complexity of the mantle, which composition is highly variable. Deciphering the source lithologies and processes involved in the OIB formation is challenging since the magmas are transformed on their way to the surface. This is especially critical at Canary Islands where the lithosphere is thought to be remarkably thick (>110 km Fullea et al., 2015). In order to better constrain the composition of primitive magmas and the plausible mantle lithologies involved, two historical eruptions recorded at Lanzarote island, Timanfaya 1730-1736 and 1824 eruptions have been investigated. Indeed, these two eruptions offer a unique opportunity to investigate the mechanisms of magma generation and composition in the context of mantle heterogeneity. The Timanfaya, 1730-1736 historical eruption emitted magmas that evolved from basanites through alkali basalts, finally reaching tholeiitic compositions at the end of the eruption. In 1824 the last eruption on the island produced extremely volatile-rich basanite. The heterogeneity of the mantle is demonstrated to the extreme in Lanzarote where a single eruption exhibits compositional variations similar to the span of the OIB worldwide. The extreme heterogeneity is systematic from whole rock lava and tephra at eruption scale but amplified at mineral and melt inclusion scale within a single tephra sample of the eruption.The use of trace element concentrations and ratios of olivine (e.g. Ni, Mn, and Ca) are valuable indicators of the mantle source lithology, namely, the fractionation-corrected Ni x (FeO/MgO) and Fe/Mn as probes of olivine absent or present lithologies, often taken as pyroxenite-derived component in mixtures of primary melts. The measured trace element concentrations in olivine from the 1730-1736 and 1824 eruptions reveal variable mantle lithologies involved in the magma generation with time. Higher Ni and lower Mn and Ca contents are expected when melting Ol-free source, such as pyroxenite lithologies. The basanites exhibit the largest variation covering the range of olivine in MORB and OIB worldwide whereas later produced alkali-basalts and tholeites have values typically expected from pyroxenite derived melts. The Fo content decreases systematically with time during the 1730-36 eruption and the proportion of silica-saturated primary melt increased in the parental magma mixture with time. At the end of the eruption, tholeiite magmas crystallized olivine with lower Fo content, whereas those concentrations of Mn and Ca increased together with Ca/Al at relatively uniform Ni x (FeO/MgO) and Fe/Mn, all of which is readily explained by increased decompression melting at slightly lower temperature. The basanite from the eruption that took place in 1824 has olivine with the highest Fo content and trace element variability expanding the range of the Timanfaya basanite. The fact that Lanzarote basanites contain olivine with trace element systematic spanning that of MORB and pyroxenite melt is explained by CO2-flux melting of a lithologically heterogeneous source, generating the diverse compositions. In addition, early reactive porous flow through the depleted oceanic lithosphere and equilibration with harzburgite restite caused Ni depletion of the earliest percolating pyroxenite melt from which olivine crystallized and probably leaving dunite channels. After the channel formation mantle nodules could be brought to the surface. The fact that olivine compositions and basanite magma were reproduced approximately a century later may reflect episodic carbonatic fluxing in the slowly uprising Canarian mantle plume. (...)
Peterman, Kenneth James. "Determination of Oxygen Fugacity using Olivine-Melt Equilibrium: Implications for the Redox States of Mid-Ocean Ridge Basalt and Ocean Island Basalt Mantle Source Regions." The Ohio State University, 2017. http://rave.ohiolink.edu/etdc/view?acc_num=osu1502803559889083.
Повний текст джерелаSimonetti, Antonio Carleton University Dissertation Earth Sciences. "Comparative Nd, Pb, and Sr isotopic study of alkalic complexes from East Africa and India; implications for mantle source regions, melt dynamics and fluid processes." Ottawa, 1994.
Знайти повний текст джерелаMollex, Gaëlle. "Architecture de la plomberie du volcan carbonatitique Oldoinyo Lengai : nouvelles contraintes sur la source, les transferts hydrothermaux, et la différenciation magmatique dans la chambre active." Thesis, Université de Lorraine, 2017. http://www.theses.fr/2017LORR0123/document.
Повний текст джерелаThe uniqueness of Oldoinyo Lengai to emit natrocarbonatite lavas makes this volcano a natural laboratory to study the genesis of these magmas. New helium isotopic data permit to assert that the signature of the fumaroles has been constant since 1988 despite the radical morphological change of the summit crater after the last sub-Plinian eruption in 2007-2008. The alternation of the effusive and explosive eruptions does not cause major modifications in the hydrothermal system architecture, which is inferred to be deeply rooted. Cognate xenoliths that were emitted during the eruption in 2007-2008 represent a unique opportunity to document the igneous processes occurring within the active magma chamber. The comparison between the noble gas (helium) isotopic compositions of the active magma chamber and those of the other silicate volcanoes of the Arusha region indicates that both types of magmatism have similar sources, identified as being a typical sub-continental lithospheric mantle, which was previously metasomatized by asthenospheric fluids. Moreover, these isotopic signatures confirm that no crustal contamination has occurred during the magma ascent from the mantle to the surface. Detailed petrographic descriptions coupled to a thermo-barometric approach, and to the determination of volatile solubility models for a phonolite composition, allow us to identify the melt evolution at magma chamber conditions and the storage parameters. These results indicate that the magma injected in 2007 has a phonolitic composition and contains a high amount of volatiles (3.2 wt.% H2O and 1.4 wt.% CO2) as well as a temperature around 1060° C. This magma subsequently evolved in the crustal magma chamber located at 11.5 ± 3.5 km depth until reaching a nephelinite composition and a temperature of 880°C. During the differentiation in the magma chamber, the silicate magma is enriched in calcium, sodium, magnesium and iron, whereas the content of silicate, potassium and aluminum decreases. Our results support previous studies related to this eruption, and are similar to the historical products emitted during the whole volcano history, permitting the suggestion that no major modification in the plumbing system has occurred during the Oldoinyo Lengai evolution. The trace elements (REE, LILE and HFSE) measured in the minerals and melt inclusions reveal a concentration reaching 100 to 1000 times the primitive mantle composition. A preliminary experimental study based on the recharge melt composition (phonolite) and identified magma chamber conditions (P, T) permits to reproduce the immiscibility between silicate and carbonatite liquids, key processes at the origin of the Oldoinyo Lengai carbonatites. The continuation of this experimental study will lead to a better comprehension of the carbonatite genesis, thus improving our understanding of the processes that are responsible for the enrichment in trace elements
Valer, Marina. "Origine et évolution des magmas de l'île de la Réunion : apports de la pétro-géochimie et des inclusions magmatiques." Thesis, Clermont-Ferrand 2, 2016. http://www.theses.fr/2016CLF22775/document.
Повний текст джерелаDespite the isotopic homogeneity of the La Réunion lavas, a petrographic and chemical diversity is observed in the products of the two main volcanoes of the island, le Piton des Neiges and le Piton de la Fournaise. Although the majority of the lavas are transitional basalts which are mainly controlled by olivine fractionation and/or accumulation, some relatively old lavas show petrological and geochemical characteristics that reflect various and relatively complex magmatic conditions, as well as storage and plumbing systems. This is for instance the case of the Plagioclase Ultraphyric-Basalts, basalts from the eccentric ‘adventive’ cones and from the Hudson crater (1998 eruption), on which this works deals with. The petro-geochemical study of the lavas is coupled with the investigation of naturally vitreous or experimentally quenched mineral-hosted melt inclusions, in order to characterize the origin of the magmas and their evolution processes in an oceanic hotspot context. The incompatible trace element ratios of the melt inclusions trapped within early-formed olivine crystals (Fo > 85) from the adventive cones are used to identify the nature of the La Réunion mantle plume source. The results suggest that magmas of the adventive cones originate from chemical source comparable to that of all the La Réunion lavas. This source is intermediate between a primitive-like mantle domain and a depleted one, almost unaffected by recycling processes. Small degrees of melting of this source can explain the enriched trace element concentrations of the melt inclusions. Plagioclase-bearing ultraphyric basalts, which can have up to 35 % millimetre-sized plagioclase crystals, were erupted during some stages of building of the two volcanoes. The compositions of the melt inclusions hosted in the plagioclase macrocrystals (An 84.2-71.7 ) and textural observations of the crystals highlight their inherited character. The parental melts of the crystals mainly evolve by clinopyroxene and plagioclase crystallization. Density contrasts between the phases allow plagioclase segregation by flotation and their accumulation at the top of the chamber. The Plagioclase Ultraphyric-Basalts are derived from the remobilization of this plagioclase-rich accumulation zones, upon input of a new batch of magma. The specific eruption periods of these basalts would correspond to decreases in the magma supply, which promoted plagioclase crystallization. Lava textures of the adventive cones and Hudson crater and their olivine-hosted melt inclusions reflect a complex history of the crystals, and the role of recycling processes in the magma feeding system of the Piton de la Fournaise volcano. The olivine crystals are clearly more magnesian (Fo > 85) than those found in the historical lava ones. The chemical compositions of the lavas show that they correspond for the most part to slightly alkaline basalts, called “Mid-Alkaline Basalts”, which are depleted in CaO and enriched in compatible and incompatible elements. Isotopic and trace element compositions suggest that they have a common origin with the historical lavas, but partial melting degrees are lower for the “Mid-Alkaline Basalts”. Clinopyroxene and plagioclase deep fractionation would explain their formation. All the results suggest that the ascent of deep-seated magma clearly could bypass the central volcanic system
Sorbadère, Fanny. "Apport des inclusions magmatiques et de la fusion expérimentale d'une source mixte péridotite-pyroxénite à l'étude des mécanismes de genèse des magmas d'arc sous-saturés en silice." Phd thesis, Université Blaise Pascal - Clermont-Ferrand II, 2013. http://tel.archives-ouvertes.fr/tel-00814866.
Повний текст джерелаLea, Emma J. "Moving from meat : vegetarianism, beliefs and information sources." Connect to this title online, 2001. http://web4.library.adelaide.edu.au/theses/09PH/09phl4335.pdf.
Повний текст джерелаNarciso-Gaytan, Carlos. "Dietary lipid source and vitamin e influence on chicken meat quality and lipid oxidation stability." Thesis, [College Station, Tex. : Texas A&M University, 2008. http://hdl.handle.net/1969.1/ETD-TAMU-2746.
Повний текст джерелаValantin, Muriel. "Fécondation, environnement climatique, équilibre source-puits et qualité du melon cantaloup charentais (cucumis melo L. )." Aix-Marseille 3, 1998. http://www.theses.fr/1998AIX30023.
Повний текст джерелаGennaro, Mimma Emanuela. "Sulfur behavior and redox conditions in Etnean hydrous basalts inferred from melt inclusions and experimental glasses." Thesis, Orléans, 2017. http://www.theses.fr/2017ORLE2005/document.
Повний текст джерелаSulfur is an important volatile component of magmas that presents different oxidation states, depending on the redox conditions and on the phase of occurrence: in silicate melts it is typically dissolved as S⁶⁺ and/or S²⁻ , in the gas phase it occurs principally as SO₂ (S⁴⁺ ) and H₂S (S²⁻). Mount Etna, in which magmatic redox conditions are poorly constrained, is used as a case study to investigate sulfur behavior in hydrous basaltic magmas during magma differentiation and degassing. This research integrates the study of natural olivine-hosted melt inclusions with an experimental study on S solubility in hydrous alkali basalts at magmatic conditions.Experimental results suggest the important control of ƒO₂ on the S abundance in Etnean hydrous magma and its partitioning between fluid and melt phases. Melt inclusions were entrapped at different depths inside the magmatic system (up to ~ 18 km, below crater level). They delineate a continuous differentiation trend, marked by fractional crystallization, from the picritic basalt (FS) toward the most evolved and degassed (2013) basalt. S content in Etnean melt is extremely variable and reaches 4150 ppm in the primitive melt inclusions. XANES Fe³⁺/ΣFe spectra in some glass inclusions, resulted in the generally decreasing of Fe³⁺/ΣFe ratios from the most primitive (FS) to the most evolved (2013) melts. MELTS software confirms that the Fe³⁺/ΣFe decrease is due principally to the melt differentiation process, enhanced to the S degassing at ƒO₂ < NNO+1. Magma reduction, in turn, induces the decrease of the sulfur solubility in the hydrous Etnean basalt, as well as of the sulfide saturation, and may constitute a possible enhancer of S exsolution, triggering the important S degassing observed in the last decades in Mt. Etna
Книги з теми "Melt source"
Berry, Brad W. Meat freezing: A source book. Amsterdam: Elsevier, 1989.
Знайти повний текст джерелаTo meet at the source: Hindus & Quakers. Wallingford, Pa: Pendle Hill Publications, 1989.
Знайти повний текст джерелаTaylor, C. Michael. Meet the registrar: Firsthand accounts of ISO 9000 success from the Registration source. Milwaukee, Wis: ASQC Quality Press, 1997.
Знайти повний текст джерелаVișoianu, Constantin. Misiunile mele: Culegere de documente. București: Editura Enciclopedia, 1997.
Знайти повний текст джерелаDr, Singh K. K., Mathur A. N. 1945-, Rathore N. S. 1960-, and India. Dept. of Non-Conventional Energy Sources., eds. Advances in biomass gasification technology: Proceeding of IInd national MEET/PICCOP meet, December 20-21, 1990. Udaipur, Rajasthan: Himanshu Publications, 1991.
Знайти повний текст джерелаElzufon, Betsy. Residential and commercial source control programs to meet water quality goals: Project 95-IRM-1, 1998. Alexandria, VA: Water Environment Research Foundation, 1998.
Знайти повний текст джерелаTomisa, Ilona. "Mely hív szolgálattyáért Esztendőbéli fizetése lészen": Szemelvények a Dessewffy család XVIII. századi gazdasági irataiból. Budapest: L' Harmattan, 2003.
Знайти повний текст джерелаSkuodis, Vytautas. Melo, neapykantos ir šmeižto kronika, 1993-1997 metai. Vilnius: Gairės, 2007.
Знайти повний текст джерелаEnding the energy stalemate: A bipartisan strategy to meet America's energy challenges. [Washington, DC]: National Commission on Energy Policy, 2004.
Знайти повний текст джерелаBreviarium caeremoniarum monasterii Mellicensis. Siegburg: Apud Franciscum Schmitt Success., 1987.
Знайти повний текст джерелаЧастини книг з теми "Melt source"
Percival, J. A. "Melt-Induced Fluid Pumping and the Source of CO2 in Granulites." In Fluid Movements — Element Transport and the Composition of the Deep Crust, 61–69. Dordrecht: Springer Netherlands, 1989. http://dx.doi.org/10.1007/978-94-009-0991-5_6.
Повний текст джерелаWang, Bitong, Andrew Caldwell, Antoine Allanore, and Douglas H. Kelley. "Investigation of Echo Source and Signal Deterioration in Ultrasound Measurement of Metal Melt." In The Minerals, Metals & Materials Series, 495–506. Cham: Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-030-92381-5_46.
Повний текст джерелаBehera, Bhuban M., V. Thirukumaran, Neeraj Kumar Sharma, and Tapas Kumar Biswal. "A Preliminary Study on Earthquake Source Properties Based on Geochemistry, Shear Resistance and Melt Pressure of Pseudotachylites, Gangavalli Fault, South India." In Society of Earth Scientists Series, 175–97. Cham: Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-40593-9_8.
Повний текст джерелаBanerjee, Rituparna, Arun K. Verma, B. M. Naveena, and V. V. Kulkarni. "Processing, Storage, and Transportation of Meat and Meat Products." In Animal Sourced Foods for Developing Economies, 77–117. Boca Raton, FL : Taylor & Francis, 2019. | Series: World Food Preservation Center book series: CRC Press, 2018. http://dx.doi.org/10.1201/9780429398575-5.
Повний текст джерелаMukherjee, Sudipta. "Meet Roslyn Syntax API." In Source Code Analytics With Roslyn and JavaScript Data Visualization, 1–14. Berkeley, CA: Apress, 2016. http://dx.doi.org/10.1007/978-1-4842-1925-6_1.
Повний текст джерелаAzimova, Shakhnoza S., and Anna I. Glushenkova. "Cucumis melo L." In Lipids, Lipophilic Components and Essential Oils from Plant Sources, 294–96. London: Springer London, 2012. http://dx.doi.org/10.1007/978-0-85729-323-7_931.
Повний текст джерелаSchmidt, H. "Impurities in Meat — Sources and Influences." In Safeguarding Food Quality, 147–56. Berlin, Heidelberg: Springer Berlin Heidelberg, 1993. http://dx.doi.org/10.1007/978-3-642-78025-7_13.
Повний текст джерелаAzimova, Shakhnoza S., and Anna I. Glushenkova. "Melo sativus Sageret ex M. Roem. (Cucumis melo L., C. chaete Wall.)." In Lipids, Lipophilic Components and Essential Oils from Plant Sources, 316. London: Springer London, 2012. http://dx.doi.org/10.1007/978-0-85729-323-7_977.
Повний текст джерелаJobling, A. "Food proteins from red meat by-products." In New and Developing Sources of Food Proteins, 31–50. Boston, MA: Springer US, 1994. http://dx.doi.org/10.1007/978-1-4615-2652-0_2.
Повний текст джерелаDelgado, Amélia Martins, Salvatore Parisi, and Maria Daniel Vaz Almeida. "Fish, Meat and Other Animal Protein Sources." In Chemistry of the Mediterranean Diet, 177–207. Cham: Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-29370-7_7.
Повний текст джерелаТези доповідей конференцій з теми "Melt source"
Tovey, Madeline, Andrea Giuliani, David Phillips, Chiranjeeb Sarkar, Graham Pearson, Tom Nowicki, and Jon Carlson. "Decoupling of Kimberlite Source and Primitive Melt Compositions." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.2618.
Повний текст джерелаBöhnke, Mischa, Felix Genske, and Andreas Stracke. "Mantle Source Heterogeneity Inferred from Olivine-Hosted Melt Inclusions." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.214.
Повний текст джерелаRosseel, E., J. P. Lu, A. Hikavyy, P. Verheyen, T. Hoffmann, O. Richard, J. Geypen, et al. "Impact of sub-melt laser annealing on Si1-xGex source /drain defectivity." In 2007 15th International Conference on Advanced Thermal Processing of Semiconductors. IEEE, 2007. http://dx.doi.org/10.1109/rtp.2007.4383859.
Повний текст джерелаNemchinsky, Valerian. "Melting Rate of a Solid With Periodic Melt Removal." In ASME 1999 International Mechanical Engineering Congress and Exposition. American Society of Mechanical Engineers, 1999. http://dx.doi.org/10.1115/imece1999-1035.
Повний текст джерелаLuo, Zhibo, and Yaoyao Fiona Zhao. "Finite Element Thermal Analysis of Melt Pool in Selective Laser Melting Process." In ASME 2018 International Design Engineering Technical Conferences and Computers and Information in Engineering Conference. American Society of Mechanical Engineers, 2018. http://dx.doi.org/10.1115/detc2018-85701.
Повний текст джерелаItoh, Hiroto, Xiaoyu Zheng, Hitoshi Tamaki, and Yu Maruyama. "Influence of In-Vessel Melt Progression on Uncertainty of Source Term During a Severe Accident." In 2014 22nd International Conference on Nuclear Engineering. American Society of Mechanical Engineers, 2014. http://dx.doi.org/10.1115/icone22-30012.
Повний текст джерелаBracco Gartner, Antoine, Igor Nikogosian, Jan Aartsen, Cathy Gonggrijp, Natascia Luciani, Gareth Davies, and Janne Koornneef. "The mantle source of lamproites from Torre Alfina, Italy: Evidence from melt inclusions in olivine." In Goldschmidt2022. France: European Association of Geochemistry, 2022. http://dx.doi.org/10.46427/gold2022.11161.
Повний текст джерелаKhoury, Regina, Celestine N. Mercer, Albert Hofstra, and Lisa Stillings. "Melt Inclusion Insights on Rhyolites Proposed as a Source of Economic Lithium in Clayton Valley, Nevada." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.1290.
Повний текст джерелаJiang, Peng, Michael Perfit, Molly Anderson, George Kamenov, and Andres Trucco. "“Probing” mantle source compositions and melt evolution beneath the northern East Pacific Rise using olivine geochemistry." In Goldschmidt2022. France: European Association of Geochemistry, 2022. http://dx.doi.org/10.46427/gold2022.12772.
Повний текст джерелаZhang, Yaqi, Vadim Shapiro, and Paul Witherell. "A Neighborhood-Based Neural Network for Melt Pool Prediction and Control." In ASME 2020 International Design Engineering Technical Conferences and Computers and Information in Engineering Conference. American Society of Mechanical Engineers, 2020. http://dx.doi.org/10.1115/detc2020-22549.
Повний текст джерелаЗвіти організацій з теми "Melt source"
Stone, M. E., and D. P. Lambert. Feed Preparation for Source of Alkali Melt Rate Tests. Office of Scientific and Technical Information (OSTI), February 2005. http://dx.doi.org/10.2172/881519.
Повний текст джерелаForsberg, C. W., G. W. Parker, J. C. Rudolph, I. W. Osborne-Lee, and M. A. Kenton. Termination of light-water reactor core-melt accidents with a chemical core catcher: the core-melt source reduction system (COMSORS). Office of Scientific and Technical Information (OSTI), September 1996. http://dx.doi.org/10.2172/453914.
Повний текст джерелаSmith, M. The Impact of the Source of Alkali on Sludge Batch 3 Melt Rate (U). Office of Scientific and Technical Information (OSTI), April 2005. http://dx.doi.org/10.2172/890167.
Повний текст джерелаLever, James, Susan Taylor, Garrett Hoch, and Charles Daghlian. Evidence that abrasion can govern snow kinetic friction. Engineer Research and Development Center (U.S.), December 2021. http://dx.doi.org/10.21079/11681/42646.
Повний текст джерелаMohammadi, N., D. Corrigan, A. A. Sappin, and N. Rayner. Evidence for a Neoarchean to earliest-Paleoproterozoic mantle metasomatic event prior to formation of the Mesoproterozoic-age Strange Lake REE deposit, Newfoundland and Labrador, and Quebec, Canada. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/330866.
Повний текст джерелаJacques, I. J., A. J. Anderson, and S. G. Nielsen. The geochemistry of thallium and its isotopes in rare-element pegmatites. Natural Resources Canada/CMSS/Information Management, 2021. http://dx.doi.org/10.4095/328983.
Повний текст джерелаConnors, Caitlin, Melanie Cohen, Sam Saint-Warrens, Fan Sissoko, Francesca Allen, Harry Cerasale, Elina Halonen, Nicole Afonso Alves Calistri, and Claire Sheppard. Psychologies of Food Choice: Public views and experiences around meat and dairy consumption. Food Standards Agency, March 2022. http://dx.doi.org/10.46756/sci.fsa.zoc432.
Повний текст джерелаBarakat, Dr Shima, Dr Samuel Short, Dr Bernhard Strauss, and Dr Pantea Lotfian. https://www.food.gov.uk/research/research-projects/alternative-proteins-for-human-consumption. Food Standards Agency, June 2022. http://dx.doi.org/10.46756/sci.fsa.wdu243.
Повний текст джерелаLampe, Jay F., John W. Mabry, and Palmer J. Holden. Comparison of Grain Sources (Barley, White Corn, and Yellow Corn) for Swine Diets and Their Effects on Meat Quality and Production Traits. Ames (Iowa): Iowa State University, January 2004. http://dx.doi.org/10.31274/ans_air-180814-1380.
Повний текст джерелаBerkowitz, Jacob F., Christine M. VanZomeren, Jaybus J. Price, and Anthony M. Priestas. Incorporating Color Change Propensity into Dredged Material Management to Increase Beneficial Use Opportunities. Engineer Research and Development Center (U.S.), December 2020. http://dx.doi.org/10.21079/11681/39261.
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