Relevant bibliographies by topics / Magic Mountain

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

Academic literature on the topic 'Magic Mountain'

Author: Grafiati
Published: 4 June 2021
Last updated: 13 February 2022

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Journal articles on the topic "Magic Mountain"

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Viano, Carlo Augusto. "The Magic Mountain." RIVISTA DI STORIA DELLA FILOSOFIA, no. 4 (October 2017): 575–84. http://dx.doi.org/10.3280/sf2017-004003.

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Kord, Catherine, Thomas Mann, and John E. Woods. "The Magic Mountain." Antioch Review 54, no. 3 (1996): 370. http://dx.doi.org/10.2307/4613374.

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Rutten, T. "The Magic Mountain." BMJ 338, jan05 2 (January 5, 2009): a3032. http://dx.doi.org/10.1136/bmj.a3032.

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Cavanagh, H. Dwight. "The Magic Mountain." Cornea 9, no. 3 (July 1990): 183. http://dx.doi.org/10.1097/00003226-199007000-00001.

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SHORE, MILES F. "Saranac: America's Magic Mountain." American Journal of Psychiatry 143, no. 12 (December 1986): 1617–18. http://dx.doi.org/10.1176/ajp.143.12.1617.

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Barclay, William R. "Saranac: America's Magic Mountain." JAMA: The Journal of the American Medical Association 257, no. 7 (February 20, 1987): 985. http://dx.doi.org/10.1001/jama.1987.03390070105039.

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Stewart, D. H. "Mann's the Magic Mountain." Explicator 57, no. 4 (January 1999): 221–23. http://dx.doi.org/10.1080/00144949909596880.

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Ramazanova, Z. B., and M. R. Seferbekov. "MOUNTAINS AND CAVES IN THE ANDIS’ RITES OF THE SUN AND RAIN MAKING." History, Archeology and Ethnography of the Caucasus 13, no. 3 (September 15, 2017): 120–24. http://dx.doi.org/10.32653/ch133120-124.

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Mod and Bakhargan were the most revered mountains for the Andis. According to the authors, the Andis used mountains and caves, as parts of the sacred landscape, on calendar holidays and in the rites of meteorological and healing magic. Thus, rites of the sun and rain making were held here. On the mountain of Bakhargan, there was a spring with healing water. The mountain of Bakhargan was used in the ceremonies of folk medicine: praying for healing, sick people described three circles round the rocks of the sacred mountain in the counterclockwise direction. In the mythology of the Andis, the tops of the mountains were the habitat of the supreme god and mountain angels. The Andis associated mountains with legends, containing the motifs of the biblical legend of the Flood. After converting to Islam, the most revered mountains were turned into places of worship, where the rite of dhikr was conducted and alms were dealt out during the prayers. Many of the rites for changing weather were led by local religious authorities or elders. Besides the use of mountains and caves in the rites of the sun and rain making, the Andis also had other rites of meteorological magic. The most common of them was the rite with a mummer. There were also rites with the use of the skull of a stallion and a snake, probably related to zoolatry. Analysis of orolatry, meteorological and healing magic of the Andis testifies to the syncretism of their spiritual culture. This confusion of traditional beliefs and Muslim religious prescriptions is peculiar to the so-called “everyday Islam”. This syncretism was common to other peoples of Dagestan and the North Caucasus.
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On Thi My, Linh. "Symbolic Space in The Magic Mountain of Thomas Mann." Journal of Science Social Science 65, no. 8 (August 2020): 55–60. http://dx.doi.org/10.18173/2354-1067.2020-0049.

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The Magic Mountain (Der Zauerberg) of Thomas Mann is one of the masterpieces of German literature in particular, of the 20th century world literature in general. In the novel, Thomas Mann created a symbolic space with the mountain in Davos and the nursing center of Davos for tuberculosis patients. The Davos Mountain influenced by sacred mountains in Grimm's fairy tales, is an experience and challenge space for the characters of the novel, especially for Hans Castorp. The nursing center of Davos for tuberculosis patients is a space to test people' patience before the hardships of life with the obsession of disease and death, pushing people to choose: stop walking, accept defeat or continue fighting for a meaningful life.
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Heaney, James J. "Tabor and the Magic Mountain." Philosophy and Theology 4, no. 4 (1990): 385–96. http://dx.doi.org/10.5840/philtheol19904411.

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Dissertations / Theses on the topic "Magic Mountain"

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Al-Hadid, Diana. "Magic Mountain." VCU Scholars Compass, 2005. http://scholarscompass.vcu.edu/etd/827.

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My installations are propositions for an imaginary world that relies on its own internal logic, a world of believability without recognition. While the work references landscape it also emphasizes its contrivance, as it is automatically estranged in an "unnatural" gallery setting. I subvert or de-familiarize the materials and processes that I use in the service of creating a fictitious environment. My places are impossible places. They are irregular, illogical, and unstable. Our imagination can be one of most dangerous things to psychological stability as it is an inventory of all things possible, no matter how irrational or improbable. The irrational is always an option, a lingering threat. The imagination seems to hate permissions and limitations, but is nevertheless lodged within them. I want to create a sense of nonsensical logic. If all things that can be imagined are logical possibilities, I want to find the place where fantasy seems to be just barely reality. If I can't have an inherent contradiction, I'll take an apparent one.
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Shea, Gregory Thomas Francis. "A petrologic study of basalts from the Magic Mountain hydorthermal area, Southern Explorer Ridge, northeast Pacific Ocean." Thesis, University of British Columbia, 1987. http://hdl.handle.net/2429/41970.

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The Magic Mountain Hydrothermal Area (MMA) is a 5 km portion of the Southern Explorer Ridge (SER) centered at 49°46' and 130°20'W. It is a region of active hydrothermal activity located near the culmination of an unusually high standing spreading centre. Seafloor photographs, conductivity-temperature surveys and acoustic images have been used to determine the nature and extent of axial volcanism and tectonism as well as the associated hydrothermal activity. Major element and trace element whole rock analyses were obtained by x-ray flourescence spectrometry (XRF) for 25 recently formed basalts collected by submersible from the MMA. These were compared with analyses of basalts dredged from other locations on the ridge axis. The mineral phases of selected samples were analysed by electron microprobe. Basalt chemical variations observed along axis reveal that some of the MMA samples are the most highly fractionated and incompatible-element-enriched basalts so far obtained from the SER. These trends, along with variations in ridge morphology and lava flow type, indicate that the volcanism of the MMA is affected by a hot spot centred at the axial topographic high five km to the north. This hot spot may be associated with the propagation of the ridge segment. Several quantitative tests of fractional crystallization indicate that the 25 MMA basalts represent at least 13 discrete lavas derived from at least 5 distinct source magmas. Mixing between magmas is indicated by disequilibrium mineral textures and compositions observed in some samples. A relationship between hot spot activity and degree of magmatism with the location and duration of axial hydrothermal activity on spreading centres is indicated by these findings. Further investigation of these relationships as well as the relationship between the tectonic processes of ridge propagation and hot spot activity is recommended.
Science, Faculty of
Earth, Ocean and Atmospheric Sciences, Department of
Graduate
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Downey, Anna Catherine. "Cenozoic mafic to intermediate volcanism at Lava Mountain and Spring Mountain, Upper Wind River Basin, Wyoming." Thesis, Kansas State University, 2015. http://hdl.handle.net/2097/20377.

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Master of Science
Geology
Matthew E. Brueseke
The Upper Wind River Basin (UWRB) is located in north-central Wyoming, to the south of the Yellowstone National Park boundary and east of Jackson Hole. Both Lava Mountain and Spring Mountain are Quaternary volcanoes in the UWRB. Lava Mountain is a shield volcano composed of 26 separate lavas capped by a scoria cone. Spring Mountain is located about ~36 km east of Lava Mountain, north of Dubois, WY, where eruptions of basalt cut through Paleocene and Eocene strata. The goal of this study aims to reconstruct the petrogenesis of magmas erupted at both volcanoes using geochemical, petrographic, and isotopic analyses. Important local events in geologic history played a large role in the development of the UWRB. This includes a long history of ancient and Cenozoic subduction, regional extension, and also the migration of the North American plate over the Yellowstone hotspot. The few previous studies on Lava Mountain claim the rocks are mafic in composition, however this was based solely on reconnaissance geological mapping. Geochemical evidence presented in this thesis show Lava Mountain rocks range from basaltic andesite to dacite. Basaltic andesite and dacite are interstratified at the base until approximately 2774 m; the rest of the volcano is andesite. All Lava Mountain samples are largely aphanitic and crystal-poor. Conversely, at Spring Mountain, localized normal faulting controls the location of eruptions of olivine-rich basalt. Petrographic analysis for both Lava Mountain and Spring Mountain display a range of evidence for open system processes, including sieved and/or resorbed pyroxenes, olivines and feldspars, as well as xenocrysts that suggest an influence from crustal assimilation. A petrogenetic model is introduced that discusses how Lava Mountain magma production occurred via fractional crystallization of basalt to dacite, then magma mixing of basaltic andesite and dacite, coupled with small amounts of crustal assimilation, to form the locally erupted andesites. All samples, including Spring Mountain basalts, have ⁸⁷Sr/⁸⁶Sr isotopes of 0.70608 and 0.70751, with ¹⁴³Nd/¹⁴⁴Nd isotopes of 0.51149 and 0.51157 and εNd values of -18 to -22. Pb isotopes plot to the left of the Geochron and directly on to slightly above the Stacey-Kramers curve. Strontium, neodymium, and lead isotope data suggest that Spring Mountain basalts are melts of ancient (e.g., 2.8 Ga Beartooth province) lithospheric mantle. The high ⁸⁷Sr/⁸⁶Sr values and exceptionally low εNd values separate the UWRB rocks from both Yellowstone and Snake River Plain volcanics, and suggest they originated from a different magma source. Finally, thermal evidence suggests melting genesis for UWRB rocks may not be Yellowstone plume related; rather it is more likely linked to Cenozoic extension.
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Hyde, Lucia K. "Magic in the mountains: selected writings on people and places in West Virginia." Thesis, Boston University, 1999. https://hdl.handle.net/2144/27679.

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Boston University. University Professors Program Senior theses.
PLEASE NOTE: Boston University Libraries did not receive an Authorization To Manage form for this thesis. It is therefore not openly accessible, though it may be available by request. If you are the author or principal advisor of this work and would like to request open access for it, please contact us at open-help@bu.edu. Thank you.
2031-01-02
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Cai, Keda, and 蔡克大. "Magmatism and tectonic evolution of the Chinese Altai, NW China: insights from the paleozoic mafic andfelsic intrusions." Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 2011. http://hub.hku.hk/bib/B47147192.

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Hobbs, Jasper. "Petrologic constraints of Cambrian mafic to intermediate volcanism in the Southern Oklahoma Aulacogen." Thesis, Kansas State University, 2015. http://hdl.handle.net/2097/18953.

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Master of Science
Department of Geology
Matthew Brueseke
The Southern Oklahoma Aulacogen (SOA) produced more than 250,000 km[superscript]3 of Cambrian mafic to silicic magmatism, associated with the opening of the Iapetus Ocean. In the Arbuckle Mountains, oil and gas exploration showed mafic to intermediate volcanic rock interbedded with rhyolite lavas. The first description of these lavas was a result of the 1982 drilling of the Hamilton Brothers Turner Falls well. Cuttings have been collected from this well and five others, and whole rock major and trace element analysis, Sr and Nd isotope analysis, and rare earth element analysis has been completed on these samples. These samples plot primarily as tholeiitic to transitional basalts to andesites. Trace element ratios show Zr/Nb values ranging from 8-10, K/Nb values ranging from 300-600, and Ba/Nb values ranging from 10-20, which overlap with known EM1 OIB values. Applying a conservative age of 535 Ma for these rocks yields [superscript]87Sr/[superscript]86Sr[subscript]i values of 0.703970 to 0.706403 and epsilon Nd values of 1.67 to 3.22, which also fall within the accepted range of EMI values. [superscript]87Sr/[superscript]86Sr[subscript]i increases with wt. % SiO[subscript]2 and K/P, consistent with the generation of evolved compositions via open-system processes. The sample with the least radiogenic Sr isotope ratio, combined with its trace element ratios is most consistent with an EM1-type source. These results, coupled with existing isotope and trace element constraints from regionally exposed dikes and plutonic rocks that crop out in the Wichita Mts., give better insight into understanding what tectonic model (lower-mantle derived hotspot or extension of the lithosphere) drove the magmatic production of the SOA. The results are more consistent with a lower-mantle origin for SOA mafic-intermediate magmatism, and indicate the potential for flood basalt volcanism.
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Allen, Tara Laine. "Mafic Alkaline Magmatism in the East Tintic Mountains, West-Central Utah: Implications for a Late Oligocene Transition from Subduction to Extension." BYU ScholarsArchive, 2012. https://scholarsarchive.byu.edu/etd/2938.

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Voluminous Eocene to Oligocene intermediate to silicic volcanic rocks related to subduction erupted throughout the Great Basin and were supplanted by bimodal eruptions of basalt and rhyolite related to extension in the Miocene. Locally, in the northern East Tintic Mountains of central Utah, this important transition is marked by a distinctive package of mafic alkaline magmas that reveal important details about the nature of this fundamental change. A late Oligocene anorthoclase-bearing shoshonite lava in the Boulter Peak quadrangle contains megacrysts of anorthoclase, with phenocrysts of olivine, clinopyroxene, magnesiohastingsite, magnetite, and apatite. The anorthoclase grains occur as glomerocrysts with irregular, resorbed edges, indicating they are not in equilibrium with the mafic phenocrysts in the shoshonite. They are interpreted to be xenocrysts incorporated into an ascending mafic magma that came into contact with a partially crystallized syenite. The mafic magma involved was probably derived by partial melting of the lithospheric mantle based on its high Mg/Fe ratios, magnesian phenocrysts, high water content, and high ratios of lithophile to high field strength elements. The syenite body likely crystallized from a highly differentiated melt. The 40Ar/39Ar age of the shoshonite is 25.35±0.04 Ma, and appears to represent the transition from subduction before the onset of extension (Christiansen et al., 2007). Other Oligocene mafic units in the area may represent different variations of the mafic alkaline endmember for the mixing process. The Gardison Ridge dike, a potassic alkaline basalt with an 40Ar/39Ar age of 26.3±0.3 Ma, contains olivine and clinopyroxene phenocrysts that are compositionally very similar to those found in the shoshonite. Other mafic dikes have even higher alkalis. All of these dikes have similar trace element patterns, with negative Nb and positive Pb anomalies, and high Ba and K concentrations. The minette of Black Rock Canyon (28.45±0.13 Ma) also contains high alkalis, particularly K, and its trace element pattern shows positive Ba and negative Nb anomalies. The clinopyroxene phenocrysts in the minette are also very similar to those found in the other alkaline rocks. The high water contents of these units are evidenced by amphibole in the shoshonite, phlogopite in the minette, and the lack of plagioclase phenocrysts in the basaltic dikes. The ages, mineral assemblages, and chemical compositions show that these late Oligocene alkaline magmas formed after a shallowly subducting oceanic slab peeled away from the overlying continental lithosphere and rolled back. Hot asthenosphere flowed in to replace the subducting plate and caused partial melting of the variably metasomatized lithospheric mantle. These alkaline magmas include the shoshonite, mafic alkaline dikes, and minette of Boulter Peak; they mark the transition from older subduction-related magmatism to Miocene magmatism caused by lithospheric extension.
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Summers, Michael Alan. "The geochemistry and petrogenesis of palaeoproterozoic mafic and ultramafic intrusions of the central Laramie mountains, Wyoming Archaean Province, USA." Thesis, University of Portsmouth, 1997. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.310469.

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Bulen, Casey L. "The role of magmatism in the evolution of the Cambrian southern Oklahoma rift zone: geochemical constraints on the mafic-intermediate rocks in the Arbuckle Mountains, OK." Thesis, Kansas State University, 2012. http://hdl.handle.net/2097/14890.

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Master of Science
Department of Geology
Matthew E. Brueseke
The Southern Oklahoma rift zone (SOA), which stretches from southern Oklahoma through the Texas panhandle and into Colorado and New Mexico, contains extensive bimodal mafic-silicic magmatism related to the opening of the Iapetus Ocean during the late Precambrian and early Cambrian. Within the SOA, the subsurface in and adjacent to the Arbuckle Mountains in southern Oklahoma contains thick packages of mafic to intermediate lava flows interlayered with thick, extensive rhyolite lava flows and lesser silicic intrusive bodies, which were first described during a 1982 drill test (Hamilton Brothers Turner Falls well) in the region. Well cuttings of these units were collected from that well and three others (Pan-Am Williams D-2, Pan-Am Jarman, Pan-Am Newberry). This study is focused on these mafic-intermediate lava flows, which represent an important stage in the evolution of the SOA and provide insights into the formation and tectonomagmatic evolution of the rift zone. The estimated 210,000 km[superscript]3 of mafic rocks in the SOA were extruded as a result of the break-up of Pannotia and the formation of the failed arm of a three-armed radial rift system. Samples analyzed from the wells plot as basalts to andesites on the TAS diagram of Le Bas et al (1986) and as subalkaline-alkaline basalts to andesite-trachyandesites on the Zr/TiO[subscript]2 vs. Nb/Y diagram of Winchester and Floyd (1977). They are dominantly tholeiitic on multiple discrimination diagrams including those of Miyashiro (1974) and Irvine and Baragar (1971). The lava flows contain traits common with EMI OIB coupled with upper crustal contamination, such as Zr/Nb values ranging from 8 to 10, Ba/Nb values ranging from 10 to 20, and K/Nb values ranging from 300 to 600. Chemostratigraphic comparisons between each well reveal up to five lava flow packages within the larger mafic-intermediate sequence, at least in the vicinity of the sampled wells. When compared with intrusive mafic rocks outcropped in the Wichita Mountains, the SOA lava flows display geochemical traits most similar to those of the Roosevelt Gabbros, suggesting a possible co-genetic relationship. Overall, the whole rock chemical characteristics coupled with comparisons with other large igneous provinces (Columbia River and Oregon Plateaus, East African Rift System) indicate that the SOA lava flows are the result of flood basalt volcanism.
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Henderson, James Dinkins III. "Magic mountain : the scenic route from thriller to comedy." Thesis, 2014. http://hdl.handle.net/2152/26570.

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This report documents the creative process that resulted in the feature screenplay "Magic Mountain," including the first inspiration for a dramatic thriller, initial attempts to devise character and plot, writing and rewriting script pages, and then the radical change of genre and artistic intention toward surrealist comedy, culminating with the final sequence of rewriting during the thesis semester.
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Books on the topic "Magic Mountain"

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Books, Diamond, and Copyright Paperback Collection (Library of Congress), eds. Mountain magic. New York: Diamond Books, 1993.

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Magic Mountain. London: Orchard, 2012.

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Magic Mountain. New York, NY: Scholastic, Incorporated, 2014.

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Mountain bike magic. Mill Valley, Calif: Bicycle Books, 1991.

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Mann, Thomas. The magic mountain. New York: The Modern Library, 1992.

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Mann, Thomas. The magic mountain. London: The Folio Society, 2000.

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Saranac: America's magic mountain. New York: Paragon House, 1988.

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Saranac: America's magic mountain. Boston: Houghton Mifflin, 1986.

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Mann, Thomas. The magic mountain: A novel. New York: Vintage International, 1996.

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White, Curtis. America's magic mountain: A novel. Normal: Dalkey Archive Press, 2004.

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Book chapters on the topic "Magic Mountain"

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Colin, Westerbeck. "The Magic Mountain." In Vittorio De Sica, edited by Howard Curle and Stephen Snyder, 280–83. Toronto: University of Toronto Press, 2000. http://dx.doi.org/10.3138/9781442683136-027.

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Wiersam, Dirk J. "Mountain." In Magic of Minerals and Rocks, 10–23. Berlin, Heidelberg: Springer Berlin Heidelberg, 2004. http://dx.doi.org/10.1007/978-3-642-18695-0_2.

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Martin, Stoddard. "Intermediary: The Magic Mountain." In Orthodox Heresy, 125–38. London: Palgrave Macmillan UK, 1989. http://dx.doi.org/10.1007/978-1-349-19669-2_6.

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Meyers, Jeffrey. "Mann: The Magic Mountain." In Disease and the Novel, 1880–1960, 39–61. London: Palgrave Macmillan UK, 1985. http://dx.doi.org/10.1007/978-1-349-17783-7_4.

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Ring, Johannes, and Heidrun Behrendt. "The Magic Mountain of Allergy Research." In Allergy and Asthma in Modern Society: A Scientific Approach, 1–2. Basel: KARGER, 2006. http://dx.doi.org/10.1159/000090223.

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Herwig, Malte. "Framing the ‘Magic Mountain Malady’: the Reception of Thomas Mann’s The Magic Mountain in the Medical Community, 1924–2000." In Framing and Imagining Disease in Cultural History, 129–50. London: Palgrave Macmillan UK, 2003. http://dx.doi.org/10.1057/9780230524323_6.

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Owsley, Richard M. "The Magic Mountain: A Prelude to Engelhardt’s Phenomenology of Illness." In Reading Engelhardt, 149–62. Dordrecht: Springer Netherlands, 1997. http://dx.doi.org/10.1007/978-94-011-5530-4_9.

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Travers, Martin. "Sickness, Knowledge and the Formation of Self: The Magic Mountain." In Thomas Mann, 60–73. London: Macmillan Education UK, 1992. http://dx.doi.org/10.1007/978-1-349-21923-0_5.

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Lentin, Antony. "The Magic Mountain: Lloyd George and Hitler at the Berghof, 1936." In Lloyd George and the Lost Peace, 89–105. London: Palgrave Macmillan UK, 2001. http://dx.doi.org/10.1057/9780230511484_5.

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Engelberg, Edward. "O Altitudo! O Solitudo! Exilic Solitude and Ambiguous Ethics on The Magic Mountain." In Solitude and Its Ambiguities in Modernist Fiction, 97–116. New York: Palgrave Macmillan US, 2001. http://dx.doi.org/10.1007/978-1-137-10598-1_6.

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Conference papers on the topic "Magic Mountain"

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Har-Peled, Sariel, Amir Nayyeri, Mohammad Salavatipour, and Anastasios Sidiropoulos. "How to walk your dog in the mountains with no magic leash." In the 2012 symposuim. New York, New York, USA: ACM Press, 2012. http://dx.doi.org/10.1145/2261250.2261269.

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Constantopoulos, James T. "RAILROAD MOUNTAIN, CHAVES COUNTY, NEW MEXICO: A GEOCHEMICALLY UNIFORM, SINGLE-PHASE MAFIC DIKE EMPLACED AT THE CRATONIC MARGIN." In Joint 53rd Annual South-Central/53rd North-Central/71st Rocky Mtn GSA Section Meeting - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019sc-327749.

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Corella Santa Cruz, Carlos Rodolfo, Francisco Abraham Paz Moreno, Alexei V. Ivanov, Elena I. Demonterova, Natalia Ukhova, Galina V. Pashkova, and Alain Demant. "PETROGENESIS OF THE ALKALINE MAFIC UPPER MIOCENE-PLIOCENE VOLCANISM FROM THE SAN FRANCISCO DE BATUC BASALTIC FIELD, SONORA, MEXICO." In Joint 70th Annual Rocky Mountain GSA Section / 114th Annual Cordilleran GSA Section Meeting - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018rm-314375.

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Graves, William, Isaac Ramon, and Heather L. Lehto. "USING MAGNETICS TO APPROXIMATE THE RELATIVE AGE OF MAFIC SILLS WITHIN DAGGER MOUNTAIN IN BIG BEND NATIONAL PARK, TX." In 51st Annual GSA South-Central Section Meeting - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017sc-289391.

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Sinton, Christopher W. "A REVIEW OF EFFORTS TO DETERMINE THE TIMING OF MAFIC DIKE INTRUSION IN THE EASTERN ADIRONDACK MOUNTAINS." In 51st Annual Northeastern GSA Section Meeting. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016ne-272472.

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Smith, Veronica, and Calvin F. Miller. "GEOCHEMICAL RELATIONS BETWEEN MAFIC INTRUSIONS IN POST-PEACH SPRING TUFF DEPOSITS IN THE SOUTHERN BLACK MOUNTAINS, ARIZONA." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-306273.

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Miyagawa, Kouichi, Yoshiyuki Maruyama, Masataka Nasada, Paolo Di Carlo, Giancarlo Conti, and Valerio Cibrario. "Advanced Testing and Simulation Techniques in Handling Body Deformation." In ASME 2008 International Mechanical Engineering Congress and Exposition. ASMEDC, 2008. http://dx.doi.org/10.1115/imece2008-67408.

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Body reinforcements may have large influence in the handling perception of a professional driver. This paper presents testing and CAE techniques to approach and analyze the phenomena. A full vehicle multi body model correlated against test data was built. The model includes all vehicle subsystems: front and rear suspensions with rotating wheels and tire model in Magic Formula representation, steering line, powertrain mounting system and car body. Flexible components have been implemented for the car trimmed body, the front subframe and the rear twist beam suspension. A special vehicle set-up has been defined for the testing session, including the standard handling equipment and an advanced system measurement based on strain gauges located on the vehicle body. Strain gauge locations have been defined through support of the simulation. Several handling maneuvers (constant radius cornering, step steering at different lateral accelerations, ISO lane change and reverse ISO lane change) have been performed. Results from strain gauges have been obtained and analyzed. Advanced testing equipments are necessary to demonstrate the influence of body flexibility, which standard handling testing equipment does not allow. This represents the first step for understanding the advanced handling perception feeling due to the body deformation and for defining a systematical approach to correlate with objective measurements.
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Rack, Sierra, David Shimabukuro, Steven Skinner, and Jo Black. "HIGH-PRESSURE, HIGH-TEMPERATURE MAFIC AMPHIBOLITE OF THE CENTRAL BELT OF THE SIERRA NEVADA MOUNTAINS NEAR COLFAX, CALIFORNIA." In GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-358869.

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Helfrich, Autumn L., Veronica C. Smith, Sarah G. Williams, Eli L. Schwat, Ian P. Thompson, Nicholas P. Lang, and Calvin F. Miller. "A FIELD-BASED AND REMOTELY SENSED PERSPECTIVE OF MAFIC INTRUSIONS WITHIN MEADOW CREEK BASIN, SOUTHERN BLACK MOUNTAINS, NW AZ." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-280521.

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Xu, Xiaohui, and Walter A. Sullivan. "MECHANISMS OF STRAIN LOCALIZATION: A CASE STUDY OF MAFIC METAVOLCANIC ROCKS OF THE WESTERN HAYFORK SUBTERRANE, KLAMATH MOUNTAINS, NW CALIFORNIA." In 53rd Annual GSA Northeastern Section Meeting - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018ne-310709.

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Reports on the topic "Magic Mountain"

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Mortensen, J. K., and R. I. Thompson. A U-Pb zircon-baddeleyite age for a differentiated mafic sill in the Ogilvie Mountains, west-central Yukon Territory. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1990. http://dx.doi.org/10.4095/129065.

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