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Relevant bibliographies by topics / Spessart

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Academic literature on the topic 'Spessart'

Author: Grafiati

Published: 4 June 2021

Last updated: 14 February 2022

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Journal articles on the topic "Spessart"

1

Bäumler, Tobias, and Andreas Baumhauer. "Monobogen als Tor zum Spessart." Stahlbau 87, no. 3 (March 2018): 225–31. http://dx.doi.org/10.1002/stab.201810578.

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Okrusch, Martin, Ulrich Schüssler, Paul Van Den Bogaard, Nikola Koglin, Helene Brätz, Joachim Lorenz, Cliff Karbusicka, and Tobias Spiegl. "Isolated alkaline basalt occurrences in the northern Spessart, Germany: Outposts of the Early Miocene Vogelsberg shield volcano?" Neues Jahrbuch für Mineralogie - Abhandlungen Journal of Mineralogy and Geochemistry 196, no. 3 (July 1, 2020): 199–219. http://dx.doi.org/10.1127/njma/2020/0194.

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Four isolated occurrences of Tertiary volcanic rocks in the northern Spessart at Beilstein, Hoher Berg, Madstein and Kasselgrund are relics of volcanic vents or dikes. They display alkaline basalts (s. l.) with mainly trachybasaltic composition, which, from normative mineral contents, may be designated as nepheline-bearing alkali-olivine basalts and basanites. In part, centimetre-sized xenoliths of spinel lherzolite occur. According to Ar-Ar dating, the alkaline basalts (s. l.) from Kasselgrund have erupted at 18.1 ± 0.3 or 19.3 ± 0.4 Ma, those of Hoher Berg between c. 18 and c. 21 Ma. These ages correspond to the Vogelsberg eruption stage I. A slightly younger Ar-Ar age of 16.8 ± 0.3 Ma was recorded for the Beilstein basalt, which is in chronological accordance to the turn of Vogelsberg eruption stages II and III. Samples of all four occurrences reveal major and trace element compositions, which are different from those of the Vogelsberg basalts. Compositions of basalts of the stage III from Vogelsberg coincide most with the Spessart basalts. This signals a special position of the northern Spessart volcanic rocks either as a discrete spatial part of the Vogelsberg volcanic suite or as smaller, independent eruption centres.

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Blome-Drees, Johannes, and Michael Zeuch. "Genossenschaftliche Förderbilanz 2016 der Raiffeisenbank Main-Spessart eG." Zeitschrift für öffentliche und gemeinwirtschaftliche Unternehmen 41, no. 1-2 (2018): 81–91. http://dx.doi.org/10.5771/0344-9777-2018-1-2-81.

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Kohlwes, Heidi. "Fortbildungszentrum Orbtalschule Bad Orb – Das Kurshaus im Spessart." physiopraxis 9, no. 11/12 (November 2011): 76. http://dx.doi.org/10.1055/s-0031-1298135.

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5

Himmelsbach, Gerrit. "Nowożytny handel bydłem oraz badania nad krajobrazem kulturowym Spessart." Biuletyn Polskiej Misji Historycznej 9 (September 16, 2014): 153. http://dx.doi.org/10.12775/bpmh.2014.006.

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6

Nasir, S., M. Okrusch, H. Kreuzer, H. Lenzt, and A. H�hndorf. "Geochronology of the Spessart Crystalline Complex, Mid-German Crystalline Rise." Mineralogy and Petrology 44, no. 1-2 (1991): 39–55. http://dx.doi.org/10.1007/bf01167099.

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7

Böhn, Andreas. "Ökonomisches Wissen in Wilhelm Hauffs zyklischer Rahmenerzählung "Das Wirtshaus im Spessart"." Zeitschrift für Germanistik 16, no. 3 (January 1, 2006): 504–12. http://dx.doi.org/10.3726/92114_504.

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8

Wagner, T., and J. Lorenz. "Mineralogy of complex Co-Ni-Bi vein mineralization, Bieber deposit, Spessart, Germany." Mineralogical Magazine 66, no. 3 (June 2002): 385–407. http://dx.doi.org/10.1180/0026461026630036.

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AbstractPost-Variscan vein-type Co-Ni-Bi ores of the Bieber deposit, Spessart mountains, Germany, which are related to the Permian Kupferschiefer, have been investigated by ore microscopy, X-ray powder diffraction and electron-probe microanalysis. The samples contain a variety of ore minerals, notably skutterudite, native bismuth, cobaltite, alloclasite, niccolite, maucherite, gersdorffite, rammelsbergite/pararammelsbergite, safflorite, loellingite and emplectite. The ores display structures indicative of multiple brecciation and complex zoned arsenide assemblages. Three sequential stages of deposition are identified, which are (1) the Cu stage, (2) the main Co-Ni-Bi stage, and (3) the late stage. The arsenide minerals, notably skutterudite, diarsenides and sulpharsenides, show a large range of compositional variation in Co-Ni-Fe space. A relatively limited number of skutterudite and diarsenide compositions lie outside the compositional fields established in the literature. Skutterudite and diarsenides are characterized by a significant substitution of As by S up to 0.44 a.p.f.u. and 0.31 a.p.f.u., respectively, which is larger than the range previously reported for these minerals. Sulpharsenide compositions can be grouped into three populations, which conform to cobaltian arsenopyrite, cobaltite and gersdorffite. They display highly variable As/S ratios between 0.95:1.00 and 1.29:0.73, consistent with experimental data. Estimates of the formation temperatures, based on the presence of dendritic native bismuth and emplectite, are in the range 100–300°C, similar to different post-Variscan mineralization styles widespread in Central Europe. Comparison of the Co-Ni-Bi vein assemblage with the framework of available paragenetic information and radiometric age data for regional mineralization events indicates an age of mineralization of ~150–160 Ma for the Bieber deposit.

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Okrusch, M., J. A. Lorenz, and S. Weyer. "THE GENESIS OF SULFIDE ASSEMBLAGES IN THE FORMER WILHELMINE MINE, SPESSART, BAVARIA, GERMANY." Canadian Mineralogist 45, no. 4 (August 1, 2007): 723–50. http://dx.doi.org/10.2113/gscanmin.45.4.723.

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10

Melkonian, Michael, and Barbara Surek. "Famous algal isolates from the Spessart forest (Germany): the legacy of Dieter Mollenhauer." Algological Studies 129 (September 1, 2009): 1–23. http://dx.doi.org/10.1127/1864-1318/2009/0129-0001.

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Dissertations / Theses on the topic "Spessart"

1

Neubauer, Dieter. "Die Wettenburg in der Mainschleife bei Urphar, Main-Spessart-Kreis." Rahden/Westf. Leidorf, 2001. http://d-nb.info/987126741/04.

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2

Marx, Isabella. "Metamorphose-Entwicklung des Spessart-Kristallins, mitteleuropäische Varisziden : phasenpetrologische, mineralchemische und geochemische Untersuchungen an Metapeliten." kostenfrei, 2008. http://www.opus-bayern.de/uni-wuerzburg/volltexte/2009/3529/.

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Weichhardt-Kulessa, Katja [Verfasser], and Ingo [Akademischer Betreuer] Kowarik. "Vegetationskundliche und vegetationsgeschichtliche Untersuchungen an Mooren im Spessart und Odenwald / Katja Weichhardt-Kulessa. Betreuer: Ingo Kowarik." Berlin : Universitätsbibliothek der Technischen Universität Berlin, 2011. http://d-nb.info/1014891639/34.

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Larsen, Annegret [Verfasser]. "Past natural and anthropogenically altered sediment flux in the Spessart mountains, a central European landscape / Annegret Larsen." Kiel : Universitätsbibliothek Kiel, 2012. http://d-nb.info/1020283998/34.

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5

Rosetti, Federico. "Saldatura su acciaio superduplex ad elevato spessore." Bachelor's thesis, Alma Mater Studiorum - Università di Bologna, 2013. http://amslaurea.unibo.it/5326/.

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6

Benussi, Carolina. "Effetto dello spessore di un'inclusione termo-poro-elastica in aree vulcaniche e idrotermali." Master's thesis, Alma Mater Studiorum - Università di Bologna, 2020. http://amslaurea.unibo.it/22107/.

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I sistemi idrotermali in ambiente vulcanico rappresentano la manifestazione in superficie di processi magmatici che avvengono in profondità. Un esempio di area idrotermale ad alto rischio vulcanico è quella di Campi Flegrei, caratterizzata da frequenti fenomeni di unrest e fenomeni di vulcanismo secondario. Gli studi riguardanti gli eventi che hanno interessato la zona negli ultimi cinquanta anni, associano questi fenomeni alla presenza ed al movimento di fluidi caldi e pressurizzati nel sottosuolo in prossimità della caldera. Il modello a sorgente termo-poro-elastica si presta a descrivere questa fenomenologia, spiegando anche la presenza della sismicità che spesso accompagna gli episodi di unrest. Una sorgente TPE presente in letteratura consiste in un'inclusione posta all'interno della crosta, a forma di disco sottile. Tale inclusione è sottoposta a variazioni di temperatura e pressione di poro, mentre il mezzo circostante si trova in condizioni drenate e isoterme. Recenti studi di tomografia suggeriscono per la caldera di Campi Flegrei la presenza di uno strato dove si concentra la sismicità dell'episodio 82-84, che è compatibile con la presenza di una sorgente TPE di dimensioni equivalenti. In questa tesi proponiamo un metodo per estendere il modello di sorgente TPE a forma di disco, al caso di un'inclusione di forma cilindrica avente uno spessore arbitrario. La sorgente di forma cilindrica può infatti essere rappresentata come una sovrapposizione di più inclusioni a forma di disco, posto che questi siano abbastanza sottili. Mostreremo quindi come stimare il numero e lo spessore dei singoli elementi che permettono di ottenere una corretta rappresentazione di una inclusione TPE cilindrica. Si proverà che lo spostamento non è significativamente influenzato dalla discretizzazione ed è ben rappresentato dal modello a disco qualunque sia lo spessore della sorgente. Per la rappresentazione degli sforzi invece, la discretizzazione risulta in generale necessaria.

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Guidi, Lorenzo. "Implementazione di un algoritmo SDF per la determinazione dello spessore di componenti meccanici." Master's thesis, Alma Mater Studiorum - Università di Bologna, 2015. http://amslaurea.unibo.it/8410/.

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8

Fischer, Martin [Verfasser], Hartmut [Akademischer Betreuer] Witte, Peter [Akademischer Betreuer] Kurtz, and Bruno [Akademischer Betreuer] Spessert. "Psychophysiologische Optimierung der akustischen Emissionen von Lebensmittel verarbeitenden Geräten / Martin Fischer. Gutachter: Peter Kurtz ; Bruno Spessert. Betreuer: Hartmut Witte." Ilmenau : Universitätsbibliothek Ilmenau, 2015. http://d-nb.info/107413947X/34.

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Fischer, Martin Verfasser], Hartmut [Akademischer Betreuer] [Witte, Peter [Akademischer Betreuer] Kurtz, and Bruno [Akademischer Betreuer] Spessert. "Psychophysiologische Optimierung der akustischen Emissionen von Lebensmittel verarbeitenden Geräten / Martin Fischer. Gutachter: Peter Kurtz ; Bruno Spessert. Betreuer: Hartmut Witte." Ilmenau : Universitätsbibliothek Ilmenau, 2015. http://nbn-resolving.de/urn:nbn:de:gbv:ilm1-2015000082.

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10

Mauri, Chiara. "Studio di un sistema di misura dello spessore senza contatto di membrane nanofibrose da elettrofilatura." Master's thesis, Alma Mater Studiorum - Università di Bologna, 2014. http://amslaurea.unibo.it/7645/.

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Questo lavoro tratta lo sviluppo di un sistema di misura contactless dello spessore da applicare nel campo delle membrane ottenute tramite il processo di elettrofilatura. Il sistema è di tipo ottico e sfrutta lo spostamento dello spot di un puntatore laser, applicato con inclinazione nota, per risalire alla variazione di spessore.

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Books on the topic "Spessart"

1

Freymann, Klaus. Der Metallerzbergbau im Spessart: Ein Beitrag zur Montangeschichte des Spessart. Aschaffenburg: Geschichts- und Kunstverein Aschaffenburg, 1991.

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2

Günther, Horst. Spessart: Bilanz einer Kulturlandschaft : Dokumentation des bayerisch-hessischen Spessart-Projektes 1995. Bad Orb: Orbensien, 1996.

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3

Immermann, Karl Leberecht. Die Wunder im Spessart: Waldmärchen. Obernburg am Main: Logo, 2004.

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Tomczyk, Leonhard. Bildende Kunst im Spessart: Ein Lexikon. Hanau: CoCon, 2009.

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5

Kampfmann, Gerhard. Verkehrsgeographie und Standorttypologie der Glashütten im Spessart. Aschaffenburg: Geschichts- und Kunstverein Aschaffenburg, 1988.

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6

Okrusch, Martin. Spessart: Geologische Entwicklung und Struktur, Gesteine und Minerale. Stuttgart: Borntraeger, 2011.

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Spessart als Text: Analyse und Aneignung einer Landschaft. Hanau: CoCon-Verlag, 2008.

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8

Schücking, Levin. Der Kampf im Spessart: Erzählung aus dem Herbst 1796. Bad Orb im Spessart: Verlag Orbensien, 1998.

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9

Gernhardt, Robert. Das Wirtshaus im Spessart: Auf den Spuren Kurt Tucholskys. Bamberg: Kleebaum Verlag, 1996.

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10

Scherg, Leonhard. Jüdisches Leben im Main-Spessart-Kreis: Orte, Schauplätze, Spuren. Haigerloch: Medien und Dialog, 2000.

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Book chapters on the topic "Spessart"

1

Weber, K. "The Spessart Crystalline Complex." In Pre-Permian Geology of Central and Eastern Europe, 167–73. Berlin, Heidelberg: Springer Berlin Heidelberg, 1995. http://dx.doi.org/10.1007/978-3-642-77518-5_16.

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Weber, K. "Structural Relationship Between Saar-Nahe Basin, Odenwald, and Spessart Mts." In Pre-Permian Geology of Central and Eastern Europe, 186–89. Berlin, Heidelberg: Springer Berlin Heidelberg, 1995. http://dx.doi.org/10.1007/978-3-642-77518-5_19.

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3

"(10951) Spessart [2.99, 0.06, 9.6]." In Dictionary of Minor Planet Names, 57. Berlin, Heidelberg: Springer Berlin Heidelberg, 2006. http://dx.doi.org/10.1007/978-3-540-34361-5_499.

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4

"Spessartin m." In Wörterbuch GeoTechnik/Dictionary Geotechnical Engineering, 1038. Berlin, Heidelberg: Springer Berlin Heidelberg, 2013. http://dx.doi.org/10.1007/978-3-642-33335-4_195164.

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Day, John Kyle. "Who Wrote the Southern Manifesto?" In The Southern Manifesto. University Press of Mississippi, 2014. http://dx.doi.org/10.14325/mississippi/9781628460315.003.0004.

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Historians neither agree upon who conceived of the the Southern Manifesto nor who actually wrote it. Most of the members of the U.S. Senate’s Southern Caucus claimed to have played a part in its drafting, while some alleged that they conceived of the project in the first place. This chapter unravels the mystery over who actually wrote the Southern Manifesto, analysing the existing scholarship and presumptions toward the document. This chapter uses all of the relevant historical evidence to reveal who in the Southern Caucus are the actual authors. The evidence reveals that though the committee of Sens. Richard Russell, Jr. of Georgia, John Stennis of Mississippi, and Sam Ervin of North Carolina were the principle authors, every member of the Southern Caucus who signed the document made significant contributions, including J. William Fulbright, Spessard Holland, J. Strom Thurmond, and Price Daniel.

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Fortini Brown, Patricia. "Suitable Alliances." In The Venetian Bride, 279–89. Oxford University Press, 2021. http://dx.doi.org/10.1093/oso/9780192894571.003.0012.

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Girolamo marries off all five daughters to Friulian nobles—three to feudal lords, two to wealthy city dwellers—thus strengthening the family network of alliances. Alvise and Giovanni become priests, the latter destined to follow his uncle Michele into high church office. Girolamo’s oldest son, Sigismondo, seeks his fortune in service of the Hapsburgs. His first marriage brings him the feud of Spessa, complete with castle, in Gorizia, and a son and heir, Carlo, named after the archduke. A second marriage into a collateral Della Torre line based in imperial territory ties him ever more firmly to the Hapsburgs. Girolamo expands the castle at Villalta, grafting a seigneurial Renaissance country villa onto the medieval fortress, the complex becoming a metaphor for a feudal family that now embraces Venetian republican values. Michele is featured in Paolo Paruta’s Della perfezione della vita politica (1579), a treatise celebrating politics as civil discipline.

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