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Journal articles on the topic 'Vogelsberg'

Author: Grafiati
Published: 4 June 2021
Last updated: 6 February 2022

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1

Hottenrott, Martin, and Erlend Martini. "Vogelsberg." Schriftenreihe der Deutschen Gesellschaft für Geowissenschaften 75 (October 30, 2011): 288–302. http://dx.doi.org/10.1127/sdgg/75/2011/288.

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2

Okrusch, Martin, Ulrich Schüssler, Paul Van Den Bogaard, et al. "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 (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 a
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3

Rau, Udo. "Die Odonatenfauna des Naturschutzparkes Hoher Vogelsberg." Deutsche Entomologische Zeitschrift 13, no. 4-5 (2008): 393–446. http://dx.doi.org/10.1002/mmnd.19660130413.

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4

Volker, Frank, and Stefanie Menges. "Field Trip A (23 September 2018): geology and geomorphology of Giessen and its surrounding areas." DEUQUA Special Publications 1 (August 20, 2018): 3–13. http://dx.doi.org/10.5194/deuquasp-1-3-2018.

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Abstract. This field trip is intended to present an introduction to the geological and geomorphological evolution of Giessen and its surrounding areas (Fig. 1). The conference location of Giessen is located at the intersection of three major geological and morphological units: the Rheinisches Schiefergebirge (Rhenish Massif) to the west, the Hessische Senke (Hessian Depression) to the north and south and the Vogelsberg volcanic field to the east (Fig. 2). The rocks of the Rheinisches Schiefergebirge (Rhenish Massif) were formed during Paleozoic times, in the context of the Variscan orogeny. Do
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5

Ipsen, Detlev. "Räumliche Vergesellschaftung." PROKLA. Zeitschrift für kritische Sozialwissenschaft 17, no. 68 (1987): 113–30. http://dx.doi.org/10.32387/prokla.v17i68.1333.

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Dem Raum so sagt Simmel, hafte wenig Verhaltensbestimmen des an. Gerade deshalb zeigesich in der räumlichen Bestimmtheit die Art der Vergesellschaftung besonders deutlich. Dies ist ein Programm für ein theoriegeleitetes Verständnis räumlicher Entwicklungen undräumlich indizierter Vergesellschaftung. Diese Arbeit will für eine Theorie des Raumes Anstöße geben und nimmt dabei bewußt in Kauf, eher Vermutungen und Thesen zu formulieren, als über gesichertes Wissen zu berichten. Der Plan für ein derartiges Vorhaben begründet sich auf individuell erfahrener Praxis. Vor nunmehr fünf Jahren kam ich, a
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6

Wagner, Michael. "Peasant Movements in the Wetterau-Vogelsberg Area, 1648–1806." Philosophy and History 21, no. 1 (1988): 127–28. http://dx.doi.org/10.5840/philhist198821174.

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7

Semmel, Arno. "Lockerbraunerden, periglaziale Solifluktionsdecken und holozäne Kolluvien im Oberwald (Hoher Vogelsberg)." E&G Quaternary Science Journal 48, no. 1 (1998): 67–71. http://dx.doi.org/10.3285/eg.48.1.07.

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Abstract. The conception that the substratum of the "Lockerbraunerde" of the Hohe Vogelsberg Mountains should represent a Late-Pleistocene, periglacial aeolian sediment, is rejected. It is demonstrated primary by means of radio carbon-datings of fossil Ah-horizons that a large portion of this substratum consists of anthropogenic colluvium. Its development occured most likely already during the earlier Holocene. The findings that the "Deckschutt" and also the substratum of the "Lockerbraunerde" are representing contemporaneous developments of the Younger Dryas are substantiated,
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8

Leßmann, Bernd. "Hydrochemische und isotopenhydrologische Untersuchungen an Grundwässern aus dem Vulkangebiet Vogelsberg." Grundwasser 6, no. 2 (2001): 81–85. http://dx.doi.org/10.1007/pl00010394.

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9

Vogelsberg, John. "Rotations: The key to farm success." American Journal of Alternative Agriculture 2, no. 1 (1987): 16. http://dx.doi.org/10.1017/s0889189300001417.

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Editor's note: At conferences with a focus on scientific and political information about alternative agriculture, the live stories of how individual farmers “made the switch” from chemical intensive to low-chemical farming help us to stay in touch with the issues as the farmer sees them. At the IAA symposium, Kansas farmer John Vogelsberg told the story of his choice to make that transition, delighting the audience with his dry humor, warmth, and wisdom. Following are excerpts from his reflections.
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10

Mai, Dieter Hans, and Hans-Joachim Gregor. "Neue und interessante Arten aus dem Miozän von Salzhausen im Vogelsberg." Feddes Repertorium 93, no. 6 (2008): 405–35. http://dx.doi.org/10.1002/fedr.19820930602.

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11

BOGAARD, P. J. F. "Petrogenesis of Basanitic to Tholeiitic Volcanic Rocks from the Miocene Vogelsberg, Central Germany." Journal of Petrology 44, no. 3 (2003): 569–602. http://dx.doi.org/10.1093/petrology/44.3.569.

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12

Sherwood, Graham J. "A paleomagnetic and rock magnetic study of Tertiary volcanics from the Vogelsberg (Germany)." Physics of the Earth and Planetary Interiors 62, no. 1-2 (1990): 32–45. http://dx.doi.org/10.1016/0031-9201(90)90190-9.

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13

Braun, T., and H. Berckhemer. "Investigation of the lithosphere beneath the Vogelsberg volcanic complex with P-wave travel time residuals." Geologische Rundschau 82, no. 1 (1993): 20–29. http://dx.doi.org/10.1007/bf00563267.

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14

Witt-Eickschen, Gudrun. "Upper mantle xenoliths from alkali basalts of the Vogelsberg, Germany: implications for mantle upwelling and metasomatism." European Journal of Mineralogy 5, no. 2 (1993): 361–76. http://dx.doi.org/10.1127/ejm/5/2/0361.

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15

Baumhauer, Roland. "Basaltic Bedding Conditions of the Tertiary Brown-Coal Formation in the Rhön and Vogelsberg Area (Tertiary Basaltic Volcanoes)." Zeitschrift der Deutschen Geologischen Gesellschaft 141, no. 1 (1990): 79–86. http://dx.doi.org/10.1127/zdgg/141/1990/79.

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16

Jung, S., and P. Masberg. "Major- and trace-element systematics and isotope geochemistry of Cenozoic mafic volcanic rocks from the Vogelsberg (central Germany)." Journal of Volcanology and Geothermal Research 86, no. 1-4 (1998): 151–77. http://dx.doi.org/10.1016/s0377-0273(98)00087-0.

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17

Sander, Thomas, Susanne Konig, Gunter M. Rothe, Alwin Janssen, and Hans Weisgerber. "Genetic variation of European beech (Fagus sylvatica L.) along an altitudinal transect at mount Vogelsberg in Hesse, Germany." Molecular Ecology 9, no. 9 (2000): 1349–61. http://dx.doi.org/10.1046/j.1365-294x.2000.01014.x.

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18

Martha, Silviu O., Gernold Zulauf, Wolfgang Dörr, et al. "The Saxothuringian-Rhenohercynian boundary underneath the Vogelsberg volcanic field: evidence from basement xenoliths and U-Pb zircon data of trachyte." Zeitschrift der Deutschen Gesellschaft für Geowissenschaften 165, no. 3 (2014): 373–94. http://dx.doi.org/10.1127/1860-1804/2014/0079.

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19

Lünsdorf, Kalies, Ahlers, Dunkl, and von Eynatten. "Semi-Automated Heavy-Mineral Analysis by Raman Spectroscopy." Minerals 9, no. 7 (2019): 385. http://dx.doi.org/10.3390/min9070385.

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A significant amount of information on sedimentary provenance is encoded in the heavy minerals of a sediment or sedimentary rock. This information is commonly assessed by optically determining the heavy-mineral assemblage, potentially followed by geochemical and/or geochronological analysis of specific heavy minerals. The proposed method of semi-automated heavy-mineral analysis by Raman spectroscopy (Raman-HMA) aims to combine the objective mineral identification capabilities of Raman spectroscopy with high-resolution geochemical techniques applied to single grains. The Raman-HMA method is an
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20

Linthout, K., H. Paulick, and J. R. Wijbrans. "Provenance of basalt blocks from Roman sites in Vleuten-De Meern (the Netherlands) traced to the Tertiary Siebengebirge (Germany): a geoarchaeological quest using petrological and geochemical methods." Netherlands Journal of Geosciences - Geologie en Mijnbouw 88, no. 1 (2009): 55–74. http://dx.doi.org/10.1017/s0016774600000998.

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AbstractUnshaped basalt blocks from archaeological sites along the border of the Roman Empire (limes) in the lower Rhine area near Vleuten-De Meern (Utrecht) have been studied petrographically, analysed by XRF for major and trace elements, and dated by the 40Ar/39Ar method. The blocks are from a revetment in the bank of a fossil branch of the Rhine and a contiguous ship De Meern 4, both built around 100 AD. All nineteen blocks are alkali olivine basalt (AOB) with xenoliths of peridotite derived from the upper mantle and quartz xenocrysts from the continental crust; eighteen blocks contain reso
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21

Schmidt, Gerhard, and Jonathan Snow. "Os isotopes in mantle xenoliths from the Eifel volcanic field and the Vogelsberg (Germany): age constraints on the lithospheric mantle." Contributions to Mineralogy and Petrology 143, no. 6 (2002): 694–705. http://dx.doi.org/10.1007/s00410-002-0372-7.

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22

Cramer, Elma. "Die Tipuliden des Naturschutzparkes Hoher Vogelsberg. (Ein Beitrag zur Biologie, Ökologie und Entwicklung der Tipuliden sowie zur Kenntnis der Limoniinenlarven und -puppen)." Deutsche Entomologische Zeitschrift 15, no. 1-3 (2008): 133–232. http://dx.doi.org/10.1002/mmnd.19680150109.

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23

de Wall, H., and L. Nano. "The Use of Field Dependence of Magnetic Susceptibility for Monitoring Variations in Titanomagnetite Composition - A Case Study on Basanites from the Vogelsberg 1996 Drillhole, Germany." Studia Geophysica et Geodaetica 48, no. 4 (2004): 767–76. http://dx.doi.org/10.1023/b:sgeg.0000045482.80307.1c.

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24

Petrovský, E., and A. Kapička. "Comments on “The use of field dependence of magnetic susceptibility for monitoring variations in titanomagnetite composition - a case study on basanites from the Vogelsberg 1996 drillhole, Germany” by de Wall and Nano, Stud. Geophys. Geod., 48, 767–776." Studia Geophysica et Geodaetica 49, no. 2 (2005): 255–58. http://dx.doi.org/10.1007/s11200-005-0008-2.

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25

Ebhardt, Götz, Karl-Heinz Ehrenberg, Martin Hottenrott, Anne Kött, Bernd Leßmann, and Heinz-Dieter Nesbor. "Geologie und Hydrogeologie des südwestlichen Vogelsberges und seiner Umrahmung (Exkursion C am 19. April 2001)." Jahresberichte und Mitteilungen des Oberrheinischen Geologischen Vereins 83 (April 17, 2001): 65–87. http://dx.doi.org/10.1127/jmogv/83/2001/65.

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26

Kniepert, F. W. "Zur Phänologie und Fluktuation der Bremsen im zentraleuropäischen Mittelgebirgsraum am Beispiel des Vogelsberges (Diptera: Tabanidae)." Deutsche Entomologische Zeitschrift 28, no. 1-3 (2008): 11–27. http://dx.doi.org/10.1002/mmnd.19810280104.

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