Relevant bibliographies by topics / Amphibolis

Contents

  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers
  6. Reports

Academic literature on the topic 'Amphibolis'

Author: Grafiati
Published: 4 June 2021
Last updated: 14 February 2022

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Journal articles on the topic "Amphibolis"

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BOGDANOVA, Alyona Romanovna, Nadezhda Vladimirovna VAKHRUSHEVA, and Pavel Borisovich SHIRYAEV. "Main and rare earth elements of amphibolites of the Ray-Iz massif (Polar Urals)." NEWS of the Ural State Mining University, no. 4 (December 20, 2020): 19–27. http://dx.doi.org/10.21440/2307-2091-2020-4-19-27.

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Relevance. The Ray-Iz massif contains the Tsentralnoye chromium ore deposit and is unique in terms of variety of metamorphic rock associations. It has been studied since 1932. However, some aspects of geology and petrology in the literature are not fully covered. One of these areas is a vein series of rocks localized in ultramafic rocks. The spatial confinement of amphibolites to the Central zone of metamorphism, which is consistent with the zone of distribution of deposits and ore occurrences of chromites, determines the need for a detailed study. Purpose of work. Study of mineralogical and petrographic characteristics, as well as the geochemistry of lanthanides of amphibolites of the Ray-Iz massif (Polar Urals). Results. The study of the nature of REE distribution in rock-forming minerals made it possible to determine that the variation in the amount of REE (33–75 g/t) within one rock is associated with the quantitative content of the main minerals-concentrators. The main mineral concentrator lanthanides in garnet amphibolites is garnet, while amphibole is in garnet-free pyroxene-bearing amphibolites. Based on the results of the chemical composition of amphibole and coexisting plagioclases and amphibolite garnets, the temperature was calculated using amphiboleplagioclase by T. Holland, J. Blundy, as well as the garnet amphibolite by L. L. Perchuk geothermometers and pressure based on amphibole geobarometer by M. W. Schmidt. Conclusion. The nature of the distribution of lanthanides in the main rock-forming minerals, amphibole and garnet, has been revealed. Comparison of parameters and compositional features of amphiboles made it possible to conclude that there is a direct relationship between temperature, pressure, the sum of REE and TiO2 , as well as (La/Yb)n , in the mineral.
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Rao, Rameshwar, and Hakim Rai. "Mineral chemistry of eclogites to investigate the evolutionary metamorphic history of UHP rocks from Tso-Morari region, Ladakh, India." Journal of Nepal Geological Society 40 (December 1, 2010): 13–20. http://dx.doi.org/10.3126/jngs.v40i0.23592.

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Micro textures of metabasics from the Tso-Morari region, Ladakh were studied in order to understand the evolutionary metamorphic history of eclogites. The mineral chemistry, paragenesis of mineral inclusions in garnet, and zoning in omphacite, garnet and amphibole suggest three main metamorphic stages: (i) an eclogite stage with late blueschist facies metamorphism, (ii) a medium-pressure amphibolite facies stage, and (iii) a low-pressure amphibolite to greenschist facies stage. The high Si content in phengite, presence of rutile besides almandine-rich garnet and omphacite in eclogites indicate the attainment of high pressures. Also, the textural features and composition of amphiboles indicate that blueschist facies conditions represented by growth of glaucophane at high pressure and low temperature were followed by a lower-pressure stage of metamorphism represented by partial and in some cases complete reaction of glaucophane to calcic green amphibole such as magnesio-hornblende. The relationships define a clock-wise P-T path with the involvement of an isothermal uplift path for the eclogites and associated garnet-amphibolites of Tso-Morari region.
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Verduin, Jennifer J., Anke Seidlitz, Mike van Keulen, and Erik I. Paling. "Maximising establishment success of Amphibolis antarctica seedlings." Journal of Experimental Marine Biology and Ecology 449 (November 2013): 57–60. http://dx.doi.org/10.1016/j.jembe.2013.08.016.

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Zhang, Xiaoli, Jinxian He, Zeqiang Ren, Taotao Zhou, Wenjie Cao, and Ben Xu. "Analysis of the Submicrostructural Deformation of Amphibole in a Ductile Shear Zone Based on the TEM Technique." Journal of Nanoscience and Nanotechnology 21, no. 1 (January 1, 2021): 765–71. http://dx.doi.org/10.1166/jnn.2021.18466.

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Deformed amphibole in the plagioclase amphibolite mylonite of the Guandi Complex, Xishan, Beijing, is the research object in this study. The amphibole nanodeformation under the middle crust was analyzed using microstructural analysis and high-resolution transmission electron microscopy (TEM). Microscope observations show that the amphibolite deformations in the plagioclase amphibolite mylonite are δ and σ type porphyroclasts, and the porphyroclast tail is composed of new long-columnar crystals. Using transmission electron microscopy (TEM, and this acronyms would be defined only once), the authors observed the nanodeformation characteristics of the amphibole porphyroclast core and mantle. Dislocation tangles are dominant in the porphyroclast core, and inside the new crystal, there is little or no dislocation. Swelled new crystals surrounded by dislocation can be observed in the transition zone between the porphyroclasts and new crystals. The deformed amphibole microstructure and submicrostructure represent typical brittle–ductile transitional deformation. The deformation process can be divided into two stages: the disordered dislocation increment stage and the dislocation reduction and ordering stage. Crystalline plastic deformation occurs in the amphibole in the plagioclase amphibolite mylonite of the Xishan area, Beijing. The crystalline plastic deformation temperature in amphiboles is higher than that in plagioclase.
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Dunlop, Robert W. "Diterpenoid hydrocarbons in the sea grass Amphibolis antartica." Phytochemistry 24, no. 5 (January 1985): 977–79. http://dx.doi.org/10.1016/s0031-9422(00)83165-9.

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Waycott, Michelle, Diana I. Walker, and Sidney H. James. "Genetic uniformity in Amphibolis antarctica, a dioecious seagrass." Heredity 76, no. 6 (June 1996): 578–85. http://dx.doi.org/10.1038/hdy.1996.83.

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Wartho, Jo Anne, David C. Rex, and Philip G. Guise. "Excess argon in amphiboles linked to greenschist facies alteration in the Kamila Amphibolite Belt, Kohistan island arc system, northern Pakistan: insights from 40Ar/39Ar step-heating and acid leaching experiments." Geological Magazine 133, no. 5 (September 1996): 595–609. http://dx.doi.org/10.1017/s0016756800007871.

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AbstractA mineralogical and 4OAr/39Ar study of 13 amphibole samples in the Kamila Amphibolite Belt and Kamila Shear Zone in northern Pakistan has found a correlation between the degree of greenschist facies alteration and quantity of excess 40Ar. Additionally, there is a north–south divide with amphibole samples from the northern region showing larger degrees of gree schist facies alteration, brittle deformation, and excess 40Ar incorporation compared to the predominantly plastically deformed, less altered, amphibole samples from the Kamila Shear Zone in the south. Acid leaching of two amphiboles from the Kamila Amphibolite Belt indicates that a large proportion of the excess 40Ar is correlated with later greenschist facies alteration hases, and can be easily removed by acid etching, thus revealing acceptable regional 40Ar/39Ar plateau ages.
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Walker, D. I., and M. L. Cambridge. "An experimental assessment of the temperature responses of two sympatric seagrasses, Amphibolis antarctica and Amphibolis griffithii, in relation to their biogeography." Hydrobiologia 302, no. 1 (March 1995): 63–70. http://dx.doi.org/10.1007/bf00006399.

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Pedersen, Morten F., Eric I. Paling, and Diana I. Walker. "Nitrogen uptake and allocation in the seagrass Amphibolis antarctica." Aquatic Botany 56, no. 2 (March 1997): 105–17. http://dx.doi.org/10.1016/s0304-3770(96)01100-x.

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Gartner, A., P. Lavery, K. McMahon, A. Brearley, and H. Barwick. "Light reductions drive macroinvertebrate changes in Amphibolis griffithii seagrass habitat." Marine Ecology Progress Series 401 (February 22, 2010): 87–100. http://dx.doi.org/10.3354/meps08367.

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Dissertations / Theses on the topic "Amphibolis"

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Watson, Jeanette Esther, and mikewood@deakin edu au. "Studies on Australian hydroids the genus eudendrium and the fauna of the seagrass amphibolis." Deakin University. School of Science, 1990. http://tux.lib.deakin.edu.au./adt-VDU/public/adt-VDU20050825.121035.

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An important Athecate genus, Eudendrium, and a group of species of the Thecata, the latter ecologically related by life on a common substrate, are reviewed. Eudendrium, hitherto poorly known in Australia, comprises 17 species, including 10 undescribed species with 71% Australian, and high provincial endemicity. Eudendrium may be a shelf genus avoiding turbulent oceanic waters. Species of Eudendrium are predominantly epizoic and some gregariously settling colonies may live for five years. Identification of sterile material is refined by using the cnidome in a key to classification. The species and population dynamics of hydroid epiphytes of the endemic southern Australian marine angiosperm Amphibolis were investigated with revision of historically vexatious taxa. In contrast with the northern hemisphere, no Athecata are associated with southern Australian seagrasses. Seventeen species from eight thecate families are associated with the two species of Amphibolis, including one undescribed species, H&lecium amphibolum, and one new record for Australia, Aglaophenia postdentata. The Lineolariidae is revised and a new genus, Millardaria, erected for a species from seagrass in Madagascar. The high endemicity (58%) and host-specificity of hydroids to Amphibolis is an evolutionary consequence of isolation of the seagrass dating from break-up of the Tethyan Sea. Hydroids occur throughout the year in the Amphibolis leaf canopy with a mean annual epiphytism of 44% on A. antarctica in the eastern continent and 86% in the western continent; epiphytism is 52% on A. griffithii in the western continent. Half of the eight important species are dominant epiphytes across the southern continent but the species and order of abundance varies regionally. Most are pioneer colonists with short, repetetive life-cycles lasting from weeks to a few months. Three species epiphytise the seagrass stems but only one is a leaf-canopy dominant. The canopy community comprises small, fast-growing species or dwarfed variants of species larger in other habitats: these ecomorphically constant forms are associated only with seagrass. Strategies for survival in the harsh Amphibolis environment include adnate colonies and gonothecae adnate or recumbent to the substrate, marked strengthening of the hydrorhiza, various hydrodynamic adaptations of the hydrotheca, early maturation and production of numerous small ova.
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Iezzi, Gianluca. "Cristallochimie des amphiboles à lithium." Orléans, 2001. http://www.theses.fr/2001ORLE2035.

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Le développement de nouvelles méthodes de micro-analyse, a révélé l'importance des éléments légers dans les minéraux majeurs. Li+, cation de petite taille, peut parfois remplacer Na+, mais fréquemment iremplace Mg2+ en sites octaédriques, ce qui implique des substitutions compensatoires. Les amphiboles présentent plusieurs types de sites susceptibles d'accueillir Li+, selon les mécanismes de substitution indiqués ci-dessus. Malgré une bonne connaissance des relations d'ordre à longue distance (LRO) impliquant Li+, fournie par des échantillons naturels, les relations d'ordre à courte distance (SRO), les conditions de stabilité et les relations avec d'autres groupes d'amphiboles étaient inconnues. Un travail expérimental, en conditions hydrothermales, complété par des études en DRX, et des analyses spectrométriques, IRTF et Mössbauer a permis de combler ce manque, sur deux types d'amphiboles à Li+, la holmquistite, avec Li+ en sites [B], et la leakeite, avec Li+ en sites [C]. Les distributions cationiques dans les différents sites ont été déterminées. Les variables utilisées ont été la composition des systèmes, T, P et fO2. La holmquistite Al n'a jamais pu être obtenue dans les conditions adoptées. Par contre, l'introduction de Fe3+ dans le système stabilise sa structure. . On décrit la ferri-ferroholmquistite, amphibole très ordonnée, avec Li+ en sites [B], Fe2+ en sites [C], et Fe3+ exclusivement en sites octaédriques M(2). Les relations d'ordre à courte distance (SRO), dans les ferri-holmquistites obtenues dans différentes conditions expérimentales, et leur évolution le long du join ferro-magnésien ont aussi été étudiées. Enfin, les relations entre clinoamphiboles sodiques et clinoamphiboles à Mg-Mn-Fe-Li ont été établies. La lacune de miscibilité communément admise entre les deux groupes n'existe pas puisqu'un remplacement complet de Na+ par Li+ en sites [B] a pu être obtenu expérimentalement. Finalement, la spectrométrie IRTF montre que dans la leakeite, Li+ est ordonné en sites M(1,3), en accord avec les données précédemment obtenues sur monocristaux naturels.
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Della, Ventura Giancarlo. "Cristallochimie des richtérites de synthèse." Orléans, 1992. http://www.theses.fr/1992ORLE2015.

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Ce travail concerne la synthese et la caracterisation cristallochimique d'amphiboles de type richterite diversement substituees. Le but de cette etude est la comprehension des mecanismes d'incorporation de divers elements cationiques (ti, sr et elements de transition), et de l'anion f#, et la determination de la reponse structurale de l'amphibole a ces substitutions. Les syntheses ont ete effectuees en conditions hydrothermales, de 600 a 900c, et sous pression d'eau de 1 a 3 kbar. Il ressort de ce travail que l'impossibilite d'obtenir certaines compositions n'est pas due au choix des conditions de synthese mais a des contraintes cristallochimiques. Les phases obtenues ont ete caracterisees par drx, ftir, raman et rietveld. L'evolution des parametres de maille en fonction du rayon ionique moyen du cation present dans un site donne est en general anisotrope. Ceci peut etre explique pour les sites o(3), m(4) et t(2), en considerant leur arrangement topologique dans la structure. Par contre, pour les sites m, c'est la configuration electronique, plus que la dimension ionique qui controle le comportement de l'ion. Globalement, l'evolution du volume de maille avec le cube du rayon ionique moyen dans le site concerne est lineaire. Le titane se fixe exclusivement en site tetraedrique, en remplacement du silicium. Seul le tetraedre t(2), a deux oxygenes pontants est concerne par cette substitution. Les elements de transition ni et co se fixent en remplacement de mg, dans les sites m, mais on observe une nette preference de ces elements pour les sites m(1,3), hydroxyles. Enfin, la substitution sr-na est aleatoire dans le site m(4)
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Sergent, José. "Relations d'ordre dans les clinoamphiboles sodi-calciques de synthèse." Orléans, 2003. http://www.theses.fr/1999ORLE2068.

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Pendlebury, K. "Compositional relationships in amphibole paragenesis." Thesis, University of Manchester, 1985. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.374562.

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McCulloch, William Robert. "Metasomatism between amphibolite and metaultramafic rocks during upper amphibolite facies metamorphism, Tobacco Root Mountains, southwest Montana." PDXScholar, 1988. https://pdxscholar.library.pdx.edu/open_access_etds/3904.

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The purpose of this study is to characterize the metasomatism that has taken place as a result of the chemical incompatibility between mafic and metaultramafic bulk compositions during high-grade regional metamorphism in the Tobacco Root Mountains, southwest Montana. Metasomatism of these rocks took place by both diffusionand infiltration-dominated processes. The result of these processes are characterized mineralogically and geochemically in the rocks.
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Najorka, Jens. "Structural and thermodynamic properties of Ca-Al-bearing amphiboles." [S.l.] : [s.n.], 2001. http://deposit.ddb.de/cgi-bin/dokserv?idn=962695629.

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Reece, James John. "In-situ studies of divalent cation behaviour in amphiboles." Thesis, University of Cambridge, 2002. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.620691.

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Jannot, Séverine Schiano Pierre. "Genèse et évolution des magmas primitifs de la chaine des Puys (Massif Central): une approche par l'étude des inclusions magmatiques." Clermont-Ferrand : Université Blaise Pascal, Clermont-Ferrand 2, 2009. http://195.221.120.247/simclient/consultation/binaries/stream.asp?INSTANCE=UCFRSIM&eidmpa=DOCUMENTS_THESES_93.

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Jannot, Séverine. "Genèse et évolution des magmas primitifs de la chaîne des Puys (Massif Central) : une approche par l'étude des inclusions magmatiques." Clermont-Ferrand 2, 2005. https://tel.archives-ouvertes.fr/tel-00684061/document.

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Les basaltes émis dans la Chaîne des Puys, dernière manifestation volcanique du Massif Central, ne correspondent pas à des magmas primaires. Ces derniers ne pouvant pas être identifiés à partir des laves, une approche plus directe a été utilisée, à savoir l'étude des inclusions magmatiques piégées dans les olivines magnésiennes. Les compositions en éléments en traces de ces liquides primitifs inclus, de type basanite-basalte alcalin, seraient le résultat de différents degrés de fusion d'une source magmatique à amphibole résiduelle, c'est-à-dire au niveau du manteau lithosphérique métasomatisé. D'autre part, les liquides piégés dans les olivines d'enclaves mantelliques retrouvées dans un des volcans étudiés sont riches en silice et en alcalins. Ils représenteraient les premiers degrés de fusion d'une péridotite à 1 GPa ; sans relation pétrogénique directe avec les liquides piégés dans les olivines magmatiques et les laves émises en surface
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Books on the topic "Amphibolis"

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Amphibolie der Reflexionsbegriffe und transzendentale Reflexion: Das Amphibolie-Kapitel in Kants Kritik der reinen Vernunft. Würzburg: Königshausen & Neumann, 2012.

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A, Valetov T., and Vasilʹev Evgeniĭ Konstantinovich, eds. Upori͡a︡dochennostʹ kationov v amfibolakh. Moskva: "Nauka", 1986.

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Page, Norman J. Composition of primary postcumulus amphibole and phlogopite within an olivine cumulate in the Stillwater Complex, Montana. Washington: U.S. Geological Survey, 1987.

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Ivanovich, Lennykh Vladimir, and Ivanov Svi͡a︡toslav Nestorovich, eds. Amfiboly golubykh slant͡s︡ev Urala. Moskva: "Nauka", 1988.

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Daziano, Carlos Oscar. Las anfibolitas de la Sierra Chica de Córdoba, Argentina. [Córdoba, Argentina]: Universidad Nacional de Córdoba, 2004.

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Distanova, A. N. Amfiboly i biotity rannepaleozoĭskikh granitoidov Tuvy i Zabaĭkalʹi͡a︡. Novosibirsk: "Nauka," Sibirskoe otd-nie, 1990.

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Awdankiewicz, Honorata. Petrologia i geochemia metabazytów masywu Niedźwiedzia na bloku przedsudeckim: The petrology and geochemistry of the metabasites of the Niedźwiedź Massif in the Fore-Sudetic Block. Warszawa: Państwowy Instytut Geologiczny, 2008.

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Nijland, Teunis Gerrit. The Bamble amphibolite to granulite facies transitions zone, Norway. [Utrecht: Faculteit Aardwetenschappen der Rijksuniversiteit Utrecht, 1993.

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Virta, Robert L. The phase relationship of talc and amphiboles in a fibrous talc sample. Pittsburg, Pa: U.S. Dept. of the Interior, Bureau of Mines, 1985.

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Kukla, Christine. Strontium isotope heterogeneities in amphibolite facies, banded metasediments--a case study from the late Proterozoic Kuiseb Formation of the southern Damara Orogen, central Namibia. Windhoek, Namibia: Ministry of Mines and Energy, Geological Survey of Namibia, 1993.

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Book chapters on the topic "Amphibolis"

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Hawthorne, Frank C., and Roberta Oberti. "1. Amphiboles: Crystal Chemistry." In Amphiboles, edited by Frank C. Hawthorne, Roberta Oberti, Giancarlo Della Ventura, and Annibale Mottana, 1–54. Berlin, Boston: De Gruyter, 2007. http://dx.doi.org/10.1515/9781501508523-002.

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Hawthorne, Frank C., and Roberta Oberti. "2. Classification of the Amphiboles." In Amphiboles, edited by Frank C. Hawthorne, Roberta Oberti, Giancarlo Della Ventura, and Annibale Mottana, 55–88. Berlin, Boston: De Gruyter, 2007. http://dx.doi.org/10.1515/9781501508523-003.

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Oberti, Roberta, Giancarlo Della Ventura, and Fernando Cámara. "3. New Amphibole Compositions: Natural and Synthetic." In Amphiboles, edited by Frank C. Hawthorne, Roberta Oberti, Giancarlo Della Ventura, and Annibale Mottana, 89–124. Berlin, Boston: De Gruyter, 2007. http://dx.doi.org/10.1515/9781501508523-004.

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Oberti, Roberta, Frank C. Hawthorne, Elio Cannillo, and Fernando Cámara. "4. Long-Range Order in Amphiboles." In Amphiboles, edited by Frank C. Hawthorne, Roberta Oberti, Giancarlo Della Ventura, and Annibale Mottana, 125–72. Berlin, Boston: De Gruyter, 2007. http://dx.doi.org/10.1515/9781501508523-005.

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Hawthorne, Frank C., and Giancarlo Della Ventura. "5. Short-Range Order in Amphiboles." In Amphiboles, edited by Frank C. Hawthorne, Roberta Oberti, Giancarlo Della Ventura, and Annibale Mottana, 173–222. Berlin, Boston: De Gruyter, 2007. http://dx.doi.org/10.1515/9781501508523-006.

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Welch, Mark D., Fernando Cámara, Giancarlo Della Ventura, and Gianluca Iezzi. "6. Non-Ambient in situ Studies of Amphiboles." In Amphiboles, edited by Frank C. Hawthorne, Roberta Oberti, Giancarlo Della Ventura, and Annibale Mottana, 223–60. Berlin, Boston: De Gruyter, 2007. http://dx.doi.org/10.1515/9781501508523-007.

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Evans, Bernard W. "7. The Synthesis and Stability of Some End-Member Amphiboles." In Amphiboles, edited by Frank C. Hawthorne, Roberta Oberti, Giancarlo Della Ventura, and Annibale Mottana, 261–86. Berlin, Boston: De Gruyter, 2007. http://dx.doi.org/10.1515/9781501508523-008.

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Maresch, Walter V., and Michael Czank. "8. The Significance of the Reaction Path in Synthesizing Single-Phase Amphibole of Defined Composition." In Amphiboles, edited by Frank C. Hawthorne, Roberta Oberti, Giancarlo Della Ventura, and Annibale Mottana, 287–322. Berlin, Boston: De Gruyter, 2007. http://dx.doi.org/10.1515/9781501508523-009.

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Martin, Robert F. "9. Amphiboles in the Igneous Environment." In Amphiboles, edited by Frank C. Hawthorne, Roberta Oberti, Giancarlo Della Ventura, and Annibale Mottana, 323–58. Berlin, Boston: De Gruyter, 2007. http://dx.doi.org/10.1515/9781501508523-010.

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Schumacher, John C. "10. Metamorphic Amphiboles: Composition and Coexistence." In Amphiboles, edited by Frank C. Hawthorne, Roberta Oberti, Giancarlo Della Ventura, and Annibale Mottana, 359–416. Berlin, Boston: De Gruyter, 2007. http://dx.doi.org/10.1515/9781501508523-011.

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Conference papers on the topic "Amphibolis"

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Hostettler, Eve I., Laura E. Waters, Sarah M. Roeske, and Matty Mookerjee. "INVESTIGATING AMPHIBOLE COMPOSITIONS FROM HIGH-GRADE AMPHIBOLITE IN THE BEAR MOUNTAIN HIGH STRAIN ZONE." In 116th Annual GSA Cordilleran Section Meeting - 2020. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020cd-347198.

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Lobanov, B. M., and V. A. Zhitko. "EXPERIENCE OF RESOLVING RUSSIAN PHRASE AMPHIBOLOGES USING "INTONTRAINER" SYSTEM." In International Conference on Computational Linguistics and Intellectual Technologies "Dialogue". Russian State University for the Humanities, 2020. http://dx.doi.org/10.28995/2075-7182-2020-19-1078-1090.

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The phenomenon of amphibologies in the Russian language and methods for its resolution, in contrast to the phenomena of verbal homonymy, are still poorly studied. In this paper, it is proposed to distinguish between two classes of amphibologies—amphibole in writing and amphibole in oral speech. The main attention is paid to the consideration of the features of the manifestation of Russian-speaking oral-speech amphibologies called phrasal amphibole. The classification of phrasal amphibologies of Russian speech into the following five types is proposed: syntagmatic, accentual, intonational, verbal and homonymous. It is argued that the main differences in the semantic variants of phrasal amphibologies lie in the field of their prosodic characteristics. At the same time, the intonation of the phrase, described by the features of melodic portraits, plays the most significant role. As a means of visual comparison of melodic portraits of two semantic variants of amphibole, as well as for numerical determination of their differences, the previously developed IntonTrainer system was used.
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Matteucci, Jared, and David M. Jenkins. "CHLORINE-POTASSIUM RELATIONS IN HASTINGSITIC AMPHIBOLES." In GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-358490.

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Schnabel, Marc Aurel, and Serdar Aydin. "Amphiboly of Digital Heritage." In 2015 Digital Heritage. IEEE, 2015. http://dx.doi.org/10.1109/digitalheritage.2015.7419582.

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Metcalf, Rodney V., Brenda J. Buck, Meg Sumner-Moore, and Tomoyo Austin. "GROWTH OF FIBROUS AMPHIBOLE DURING HYDROTHERMAL ALTERATION: IMPLICATIONS FOR NON-OCCUPATIONAL EXPOSURE TO AMPHIBOLE ASBESTOS." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-282169.

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Werts, Kevin, and Calvin G. Barnes. "LINKING TEXTURAL CHARACTERISTICS OF TUOLUMNE AMPHIBOLES TO COMPOSITION AND TEMPERATURE." In 112th Annual GSA Cordilleran Section Meeting. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016cd-274457.

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Larson, Theodore, Vinicius Antao, Caroline Cusack, and Frank Bove. "Morbidity In Workers With Libby Amphibole Exposure." In American Thoracic Society 2010 International Conference, May 14-19, 2010 • New Orleans. American Thoracic Society, 2010. http://dx.doi.org/10.1164/ajrccm-conference.2010.181.1_meetingabstracts.a1741.

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Bartoli, Omar, Jean-François Moyen, Bernardo Cesare, Antonio Acosta-Vigil, and Stefano Poli. "ARCHEAN MELT INCLUSIONS IN BARBERTON AMPHIBOLITES (SOUTH AFRICA)." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-280229.

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Austin, Tomoyo, Rodney V. Metcalf, and Brenda J. Buck. "METASOMATIC MICROTEXTURES AND THE PETROGENESIS OF AMPHIBOLE ASBESTOS." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-281939.

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Jenkins, David M. "THE ROLE OF CHLORIDE TYPE ON THE SYNTHESIS OF CHLORINE-BEARING AMPHIBOLES." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-278132.

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Reports on the topic "Amphibolis"

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Mader, U. K., and R. G. Berman. Amphibole Thermobarometry: a Thermodynamic Approach. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1992. http://dx.doi.org/10.4095/133594.

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McCulloch, William. Metasomatism between amphibolite and metaultramafic rocks during upper amphibolite facies metamorphism, Tobacco Root Mountains, southwest Montana. Portland State University Library, January 2000. http://dx.doi.org/10.15760/etd.5788.

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Lauf, R. Amphibole ceramics: conceptual development and preliminary experiments. Office of Scientific and Technical Information (OSTI), August 1985. http://dx.doi.org/10.2172/5136067.

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Digel, S., and T. M. Gordon. Prehnite - Pumpellyite To Amphibolite Facies Metamorphism near Flin Flon, Manitoba. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/132572.

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Joy, B. R., M. J. Keskinen, and R. J. Newberry. Preliminary thermobarometry and microprobe mineral compositions, Fairbanks area schists and amphibolites. Alaska Division of Geological & Geophysical Surveys, 1996. http://dx.doi.org/10.14509/1736.

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Dubé, B., W. Balmer, M. Sanborn-Barrie, T. Skulski, and J. Parker. A preliminary report on amphibolite-facies, disseminated-replacement-style mineralization at the Madsen gold mine, Red Lake, Ontario. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2000. http://dx.doi.org/10.4095/211162.

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Sevigny, J. H. Field and Stratigraphic Relations of Amphibolites in the Late Proterozoic Horsethief Creek Group, northern Adams River area, British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1987. http://dx.doi.org/10.4095/122536.

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Newberry, R. J. Whole-rock and trace element analyses of two amphibolite outcrop samples from the 2001 DGGS Salcha River-Pogo project, Big Delta Quadrangle, Alaska. Alaska Division of Geological & Geophysical Surveys, November 2012. http://dx.doi.org/10.14509/24664.

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Ames, D. E., I. M. Kjarsgaard, and J. A. R. Stirling. Mineral chemistry and x-ray diffraction database of greenschist- to amphibolite-facies assemblages in the Hidden and Louis formations, Paleoproterozoic Flin Flon Domain. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2011. http://dx.doi.org/10.4095/289261.

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Ames, D. E., and G. Tuba. Epidote-amphibole and accessory phase mineral chemistry as a vector to low-sulphide platinum group element mineralization, Sudbury: laser ablation ICP-MS trace element study of hydrothermal alteration. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2015. http://dx.doi.org/10.4095/296695.

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