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Journal articles on the topic 'Bergen Arcs'

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Published: 10 December 2022

Last updated: 28 January 2023

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1

Davydova, V. V., A. L. Perchuk, and B. Stoeckhert. "Petrology of coronite from the Bergen Arcs Complex, Norway." Moscow University Geology Bulletin 64, no. 3 (June 2009): 166–76. http://dx.doi.org/10.3103/s0145875209030041.

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2

Putnis, Andrew, Bjørn Jamtveit, and Håkon Austrheim. "Metamorphic Processes and Seismicity: the Bergen Arcs as a Natural Laboratory." Journal of Petrology 58, no. 10 (October 1, 2017): 1871–98. http://dx.doi.org/10.1093/petrology/egx076.

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3

Raimbourg, Hugues, Laurent Jolivet, Loïc Labrousse, Yves Leroy, and Dov Avigad. "Kinematics of syneclogite deformation in the Bergen Arcs, Norway: implications for exhumation mechanisms." Geological Society, London, Special Publications 243, no. 1 (2005): 175–92. http://dx.doi.org/10.1144/gsl.sp.2005.243.01.13.

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4

Andersen, T., H. Austrheim, and E. A. J. Burke. "Fluid inclusions in granulites and eclogites from the Bergen Arcs, Caledonides of W. Norway." Mineralogical Magazine 54, no. 375 (June 1990): 145–58. http://dx.doi.org/10.1180/minmag.1990.054.375.02.

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AbstractThe Grenvillian granulite-facies complex on Holsnøy island, Bergen Arcs, W. Norway, has been metamorphosed at eclogite-facies conditions during the Caledonian orogeny (ca. 425 Ma). The granulite-eclogite facies transition takes place along shear zones and fluid pathways. Mineral thermobarometry indicates PT conditions of 800–900°C and 8–10 kbar for the Proterozoic granulite facies metamorphism and 700–800°C and 16–19 kbar for the eclogite-forming event. Quartz in the granulite facies complex contains CO2 fluid inclusions with less than 2.5 mole percent N2; the molar volumes are compatible with the PT conditions of the Proterozoic granulite metamorphism. Quartz in pegmatitic quartz + omphacite and quartz + phengite/paragonite veins coeval with shear-zone eclogites contain N2 ± CO2 fluid inclusions. Combined laser Raman microanalysis and microthermometry show that the least disturbed inclusions have XCO2 = 0.1–0.3, and molar volumes less than 40 cm3/mole, which may agree with the PT conditions during Caledonian high-pressure metamorphism. Younger, low-density N2 and N2-H2O fluid inclusions are the results of decrepitation and redistribution of early inclusions during the retrograde PT evolution of the eclogites.

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5

Jamtveit, Bj�rn, Kurt Bucher-Nurminen, and H�kon Austrheim. "Fluid controlled eclogitization of granulites in deep crustal shear zones, Bergen arcs, Western Norway." Contributions to Mineralogy and Petrology 104, no. 2 (February 1990): 184–93. http://dx.doi.org/10.1007/bf00306442.

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6

Boundy, T. "Temporal and tectonic evolution of the granulite-eclogite association from the Bergen Arcs, western Norway." Lithos 39, no. 3-4 (February 1997): 159–78. http://dx.doi.org/10.1016/s0024-4937(96)00026-6.

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7

Centrella, Stephen, Håkon Austrheim, and Andrew Putnis. "Mass transfer and trace element redistribution during hydration of granulites in the Bergen Arcs, Norway." Lithos 262 (October 2016): 1–10. http://dx.doi.org/10.1016/j.lithos.2016.06.019.

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8

Austrheim, Håkon, and William L. Griffin. "Shear deformation and eclogite formation within granulite-facies anorthosites of the Bergen Arcs, western Norway." Chemical Geology 50, no. 1-3 (August 1985): 267–81. http://dx.doi.org/10.1016/0009-2541(85)90124-x.

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9

Altenberger, U., and S. Wilhelm. "Ductile deformation of K-feldspar in dry eclogite facies shear zones in the Bergen Arcs, Norway." Tectonophysics 320, no. 2 (May 2000): 107–21. http://dx.doi.org/10.1016/s0040-1951(00)00048-2.

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10

Pollok, Kilian, Geoffrey E. Lloyd, Håkon Austrheim, and Andrew Putnis. "Complex replacement patterns in garnets from Bergen Arcs eclogites: A combined EBSD and analytical TEM study." Geochemistry 68, no. 2 (June 2008): 177–91. http://dx.doi.org/10.1016/j.chemer.2007.12.002.

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11

Bingen, Bernard, Håkon Austrheim, Martin J. Whitehouse, and William J. Davis. "Trace element signature and U–Pb geochronology of eclogite-facies zircon, Bergen Arcs, Caledonides of W Norway." Contributions to Mineralogy and Petrology 147, no. 6 (June 22, 2004): 671–83. http://dx.doi.org/10.1007/s00410-004-0585-z.

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12

Petley-Ragan, Arianne, Yehuda Ben-Zion, Håkon Austrheim, Benoit Ildefonse, François Renard, and Bjørn Jamtveit. "Dynamic earthquake rupture in the lower crust." Science Advances 5, no. 7 (July 2019): eaaw0913. http://dx.doi.org/10.1126/sciadv.aaw0913.

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Earthquakes in the continental crust commonly occur in the upper 15 to 20 km. Recent studies demonstrate that earthquakes also occur in the lower crust of collision zones and play a key role in metamorphic processes that modify its physical properties. However, details of the failure process and sequence of events that lead to seismic slip in the lower crust remain uncertain. Here, we present observations of a fault zone from the Bergen Arcs, western Norway, which constrain the deformation processes of lower crustal earthquakes. We show that seismic slip and associated melting are preceded by fracturing, asymmetric fragmentation, and comminution of the wall rock caused by a dynamically propagating rupture. The succession of deformation processes reported here emphasize brittle failure mechanisms in a portion of the crust that until recently was assumed to be characterized by ductile deformation.

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13

Glodny, Johannes, Alexander Kühn, and Håkon Austrheim. "Geochronology of fluid-induced eclogite and amphibolite facies metamorphic reactions in a subduction–collision system, Bergen Arcs, Norway." Contributions to Mineralogy and Petrology 156, no. 1 (December 14, 2007): 27–48. http://dx.doi.org/10.1007/s00410-007-0272-y.

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14

BOUNDY, T. M., D. M. FOUNTAIN, and H. AUSTRHEIM. "Structural development and petrofabrics of eclogite facies shear zones, Bergen Arcs, western Norway: implications for deep crustal deformational processes." Journal of Metamorphic Geology 10, no. 2 (March 1992): 127–46. http://dx.doi.org/10.1111/j.1525-1314.1992.tb00075.x.

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15

Moore, Jo, Andreas Beinlich, Jennifer K. Porter, Cristina Talavera, Jasper Berndt, Sandra Piazolo, Håkon Austrheim, and Andrew Putnis. "Microstructurally controlled trace element (Zr, U–Pb) concentrations in metamorphic rutile: An example from the amphibolites of the Bergen Arcs." Journal of Metamorphic Geology 38, no. 1 (November 25, 2019): 103–27. http://dx.doi.org/10.1111/jmg.12514.

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16

Austrheim, Håkon. "The granulite-eclogite facies transition: A comparison of experimental work and a natural occurrence in the Bergen Arcs, western Norway." Lithos 25, no. 1-3 (November 1990): 163–69. http://dx.doi.org/10.1016/0024-4937(90)90012-p.

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17

Bhowany, K., M. Hand, C. Clark, D. E. Kelsey, S. M. Reddy, M. A. Pearce, N. M. Tucker, and L. J. Morrissey. "Phase equilibria modelling constraints on P-T conditions during fluid catalysed conversion of granulite to eclogite in the Bergen Arcs, Norway." Journal of Metamorphic Geology 36, no. 3 (December 20, 2017): 315–42. http://dx.doi.org/10.1111/jmg.12294.

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18

Schneider, J., D. Bosch, P. Monié, and O. Bruguier. "Micro-scale element migration during eclogitisation in the Bergen arcs (Norway): A case study on the role of fluids and deformation." Lithos 96, no. 3-4 (July 2007): 325–52. http://dx.doi.org/10.1016/j.lithos.2006.10.001.

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19

Janots, Emilie, Håkon Austrheim, Carl Spandler, Johannes Hammerli, Claudia A. Trepmann, Jasper Berndt, Valérie Magnin, and Anthony I. S. Kemp. "Rare earth elements and Sm-Nd isotope redistribution in apatite and accessory minerals in retrogressed lower crust material (Bergen Arcs, Norway)." Chemical Geology 484 (May 2018): 120–35. http://dx.doi.org/10.1016/j.chemgeo.2017.10.007.

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20

Andersen, T., H. Austrheim, and E. A. J. Burke. "Fluid-induced retrogression of granulites in the Bergen Arcs, Caledonides of W. Norway: Fluid inclusion evidence from amphibolite-facies shear zones." Lithos 27, no. 1 (June 1991): 29–42. http://dx.doi.org/10.1016/0024-4937(91)90018-g.

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21

Centrella, Stephen. "The granulite- to eclogite- and amphibolite-facies transition: a volume and mass transfer study in the Lindås Nappe, Bergen Arcs, west Norway." Geological Society, London, Special Publications 478, no. 1 (May 21, 2018): 241–64. http://dx.doi.org/10.1144/sp478.9.

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22

Centrella, Stephen, Håkon Austrheim, and Andrew Putnis. "Coupled mass transfer through a fluid phase and volume preservation during the hydration of granulite: An example from the Bergen Arcs, Norway." Lithos 236-237 (November 2015): 245–55. http://dx.doi.org/10.1016/j.lithos.2015.09.010.

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23

Zhong, Xin, Arianne J. Petley-Ragan, Sarah H. M. Incel, Marcin Dabrowski, Niels H. Andersen, and Bjørn Jamtveit. "Lower crustal earthquake associated with highly pressurized frictional melts." Nature Geoscience 14, no. 7 (June 17, 2021): 519–25. http://dx.doi.org/10.1038/s41561-021-00760-x.

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AbstractEarthquakes at lower crustal depths are common during continental collision. However, the coseismic weakening mechanisms required to propagate an earthquake at high pressures are poorly understood. Transient high-pressure fluids or melts have been proposed as a viable mechanism, but verifying this requires direct in situ measurement of fluid or melt overpressure along fault planes that have hosted dynamic ruptures. Here, we report direct measurement of highly overpressurized frictional melts along a seismic fault surface. Using Raman spectroscopy, we identified high-pressure quartz inclusions sealed in dendritic garnets that grew from frictional melts formed by lower crustal earthquakes in the Bergen Arcs, Western Norway. Melt pressure was estimated to be 1.8–2.3 GPa on the basis of an elastic model for the quartz-in-garnet system. This is ~0.5 GPa higher than the pressure recorded by the surrounding pseudotachylyte matrix and wall rocks. The recorded melt pressure could not arise solely from the volume expansion of melting, and we propose that it was generated when melt pressure approached the maximum principal stress in a system subject to high differential stress. The associated palaeostress field demonstrates that a strong lower crust accommodated up to 1 GPa differential stress during the compressive stage of the Caledonian orogeny.

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24

Zertani, Sascha, Loic Labrousse, Timm John, Torgeir B. Andersen, and Frederik Tilmann. "The Interplay of Eclogitization and Deformation During Deep Burial of the Lower Continental Crust—A Case Study From the Bergen Arcs (Western Norway)." Tectonics 38, no. 3 (March 2019): 898–915. http://dx.doi.org/10.1029/2018tc005297.

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25

Schneider, Julie, Delphine Bosch, and Patrick Monié. "Individualization of textural and reactional microdomains in eclogites from the Bergen Arcs (Norway): Consequences for Rb/Sr and Ar/Ar radiochronometer behavior during polymetamorphism." Geochemistry, Geophysics, Geosystems 9, no. 12 (December 2008): n/a. http://dx.doi.org/10.1029/2008gc002098.

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26

Petley-Ragan, Arianne J., Oliver Plümper, Benoit Ildefonse, and Bjørn Jamtveit. "Nanoscale earthquake records preserved in plagioclase microfractures from the lower continental crust." Solid Earth 12, no. 4 (April 23, 2021): 959–69. http://dx.doi.org/10.5194/se-12-959-2021.

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Abstract. Seismic faulting causes wall rock damage, which is driven by both mechanical and thermal stress. In the lower crust, co-seismic damage increases wall rock permeability, permits fluid infiltration and triggers metamorphic reactions that transform rock rheology. Wall rock microstructures reveal high-stress conditions near earthquake faults; however, there is limited documentation on the effects of a thermal pulse coupled with fluid infiltration. Here, we present a transmission electron microscopy study of co-seismic microfractures in plagioclase feldspar from lower crustal granulites from the Bergen Arcs, Western Norway. Focused ion beam foils are collected 1.25 mm and 1.8 cm from a 1.3 mm thick eclogite facies pseudotachylyte vein. Dislocation-free plagioclase and K-feldspar aggregates in the microfractures record a history of fluid introduction and recovery from a short-lived high-stress state caused by slip along the nearby fault. The feldspar aggregates retain the crystallographic orientation of their host and are elongated subparallel to the pseudotachylyte. We propose that plagioclase partially amorphized along the microfractures at peak stress conditions followed by repolymerization to form dislocation-free grain aggregates. Repolymerization and recrystallization were enhanced by the infiltration of fluids that transported Ca and K into the microfractures. Subsequent cooling led to exsolution of intermediate plagioclase compositions and the formation of the Bøggild–Huttenlocher intergrowth in the grains from the fracture closest to the pseudotachylyte. Our findings provide unequivocal evidence that the introduction of fluids in the microfractures occurred within the timescale of the thermal perturbation, prompting rapid annealing of damaged wall rock soon after earthquake rupture.

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27

Andersen, T., H. Austrheim, and E. A. J. Burke. "Mineral-fluid-melt interactions in high-pressure shear zones in the Bergen Arcs nappe complex, Caledonides of W. Norway: Implications for the fluid regime in Caledonian eclogite-facies metamorphism." Lithos 27, no. 3 (December 1991): 187–204. http://dx.doi.org/10.1016/0024-4937(91)90012-a.

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28

Clark, Robert S. "International Festival: Bergen, Norway." Hudson Review 52, no. 3 (1999): 471. http://dx.doi.org/10.2307/3853458.

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29

Philipp, Klaus Jan. "Sainte-Waudru in Mons (Bergen, Hennegau)." Zeitschrift für Kunstgeschichte 51, no. 3 (1988): 372. http://dx.doi.org/10.2307/1482409.

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30

Shadanov, A. A., D. A. Sirota, T. A. Bergen, M. M. Lyashenko, and A. M. Chernyavskiy. "Anatomical variability in the structure of the arch and thoracic aorta and its influence on aorta related pathological conditions." Patologiya krovoobrashcheniya i kardiokhirurgiya 24, no. 4 (December 30, 2020): 72. http://dx.doi.org/10.21688/1681-3472-2020-4-72-82.

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<p><strong>Aim.</strong> Assessment of normal and variant aortic arch anatomy in patients with type A aortic dissection and aneurysm of the arch and descending thoracic aorta.</p><p><strong>Methods.</strong> We retrospectively studied computer tomography (CT) data of chest organs with contrast in patients who underwent reconstruction of the aortic arch in type I aortic dissection according to DeBakey classification (n = 61) and resection of the aortic arch and descending thoracic aorta aneurysm (n = 14) at the Meshalkin National Medical Research Center, Novosibirsk, Russian Federation. The control group included patients without aortic arch pathology (n = 52). To identify relationships between the anatomical type of aortic arch and the risk of aortic pathology development, univariate and multivariate binary logistic regression analyses were used.</p><p><strong>Results.</strong> Our analysis revealed four types of aortic arch anatomy. Normal aortic arch anatomy occurred in 66.1 % of patients (n = 84), the proportion of abnormalities of the left common carotid artery was 30 % (bovine aortic arch occurred in 15 %, and the same site of origin of left common carotid artery and brachiocephalic trunk occurred in 15 %). Divergence of the left vertebral artery from the aortic arch between the left common carotid and left subclavian arteries occurred in 3.1 % (n = 4), and the combination of “bovine trunk” and divergence of the left vertebral artery from the aortic arch was detected in 0.8 % patients (n = 1). Logistic regression analyses revealed no statistically significant relationships between variant aortic arch anatomy and the development of type A aortic dissections and aortic arch aneurysms. The presence of the common origin of brachiocephalic trunk and left common carotid artery was associated with a reduced risk of acute aortic dissection type I by 89 %, or an OR of 0.11 (95% CI: 0.03–0.46) (p = 0.002).</p><p><strong>Conclusion.</strong> Our data will help with future planning surgical interventions on the aortic arch and descending thoracic aorta.</p><p>Received 17 June 2020. Revised 16 July 2020. Accepted 17 July 2020.</p><p><strong>Funding:</strong> The study did not have sponsorship.</p><p><strong>Conflict of interest:</strong> Authors declare no conflict of interest.</p><p><strong>Author contributions</strong><br />Conception and design: A.A. Shadanov<br />Data collection and analysis: A.A. Shadanov, T.A. Bergen<br />Statistical analysis: D.A. Sirota, A.A. Shadanov<br />Drafting the article: A.A. Shadanov<br />Critical revision of the article: D.A. Sirota, M.M. Lyashenko, A.M. Chernyavskiy<br />Final approval of the version to be published: A.A. Shadanov, D.A. Sirota, T.A. Bergen, M.M. Lyashenko, A.M. Chernyavskiy</p>

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31

Ommundsen, Åslaug. "Nonneseter i Bergen – eit benediktinarkloster." Historisk tidsskrift 89, no. 04 (December 23, 2010): 547–71. http://dx.doi.org/10.18261/issn1504-2944-2010-04-03.

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32

Hobæk, Halvor. "Parametric acoustic arrays: A Bergen view." Journal of the Acoustical Society of America 125, no. 4 (April 2009): 2687. http://dx.doi.org/10.1121/1.4784268.

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33

Rifkin, Adrian. "Is Berger Burning, Still?" Journal of Visual Culture 11, no. 2 (July 25, 2012): 171–74. http://dx.doi.org/10.1177/1470412912444187o.

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34

Kristensen, Juliette. "Making Ways of Seeing: A Conversation with Mike Dibb and Richard Hollis." Journal of Visual Culture 11, no. 2 (July 25, 2012): 181–95. http://dx.doi.org/10.1177/1470412912444228.

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In 1971, Stephen Hearst, head of the BBC Music and Arts department, commissioned John Berger to make a television series on topics of his choosing. With Mike Dibb, then a young producer/director in the department, Berger made the four-part television series Ways of Seeing. Following its success, BBC Publications commissioned Berger and Dibb to turn the television programme into a book, a project for which Richard Hollis, a graphic designer Berger had previously worked with on the magazine New Society and his novel G., was brought in. Together with script consultant Chris Fox and artist Sven Blomberg, this group produced the book Ways of Seeing, jointly published by the BBC and Penguin Books in 1972. In this conversation with Juliette Kristensen, Mike Dibb and Richard Hollis discuss the history of the making of the television series and the book, Ways of Seeing.

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35

Neander, Joachim, and Alexandra-Eileen Wenck. "Zwischen Menschenhandel und "Endlosung": Das Konzentrationslager Bergen-Belsen." German Studies Review 24, no. 3 (October 2001): 629. http://dx.doi.org/10.2307/1433443.

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36

White, Jerry. "John Berger of the Haute-Savoie." Film Quarterly 70, no. 4 (2017): 93–98. http://dx.doi.org/10.1525/fq.2017.70.4.93.

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37

Jahnke, Carsten. "The German Hansa and Bergen, 1100–1600." Scandinavian Economic History Review 64, no. 1 (January 2, 2016): 72–73. http://dx.doi.org/10.1080/03585522.2015.1135186.

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38

Jedrej, Charles. "Sharif Harir, Old-Timers and New-Comers: politics and ethnicity in a Sudanese community. Bergen Occasional Papers in Social Anthropology 29. Bergen: University of Bergen, 1983, 134 pp., 0332 8147." Africa 56, no. 2 (April 1986): 258. http://dx.doi.org/10.2307/1160654.

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39

Creason, Stuart. "Biblical Hebrew and Discourse Linguistics. Robert D. Bergen." Journal of Near Eastern Studies 58, no. 2 (April 1999): 138–40. http://dx.doi.org/10.1086/468697.

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40

Sheehan, Tanya. "SEEING THROUGH RACE by Martin A. Berger." Art History 30, no. 5 (December 12, 2007): 764–69. http://dx.doi.org/10.1111/j.1467-8365.2007.00574_1.x.

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41

Dana, Jorge. "Colour by Stencil: Germaine Berger and Pathécolor." Film History: An International Journal 21, no. 2 (July 2009): 180–83. http://dx.doi.org/10.2979/fil.2009.21.2.180.

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42

Dohr, Myriam. "Nancy (Meurthe-et-Moselle). Berger-Levrault." Archéologie médiévale, no. 41 (December 1, 2011): 325–26. http://dx.doi.org/10.4000/archeomed.12919.

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43

Klüser, Ruth, and Ina Neitzner. "Die Glas- und Keramikbranche im Wandel - welche Risiken bergen anstehende Veränderungen?" Keramische Zeitschrift 71, no. 6 (November 2019): 38–45. http://dx.doi.org/10.1007/s42410-019-0079-2.

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44

Cyr, Catherine. "Jean du Berger. Le diable à la danse." Theatre Research in Canada 28, no. 1 (January 2007): 69–71. http://dx.doi.org/10.3138/tric.28.1.69.

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45

Icke-Schwalbe, Lydia. "Berger, Peter: Füttern, Speisen und Verschlingen." Anthropos 103, no. 2 (2008): 578–80. http://dx.doi.org/10.5771/0257-9774-2008-2-578.

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46

Highmore, Ben. "‘Then Turn the Page’: Berger by the Book." Journal of Visual Culture 11, no. 2 (July 25, 2012): 124–26. http://dx.doi.org/10.1177/1470412912444187a.

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47

Bar-Levav, Avriel, Rachel Rojanski, Andrea Schatz, and Irene Zwiep. "Obituary Professor Shlomo Berger (1953–2015)." Zutot 13, no. 1 (March 11, 2016): 1–3. http://dx.doi.org/10.1163/18750214-12341280.

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48

Hrabovskyi, Volodymyr. "COMPOSER VERSUS PHILOSOPHER About Roman Berger." Ukrainian music 40, no. 2 (2021): 102–4. http://dx.doi.org/10.32782/2224-0926-2021-2-11.

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49

Thun, Eirunn, Bjørn Bjorvatn, Theresa Osland, Vidar Martin Steen, Børge Sivertsen, Torill Johansen, Tom Halvor Lilleholt, Idalill Udnes, Inger Hilde Nordhus, and Ståle Pallesen. "An Actigraphic Validation Study of Seven Morningness-Eveningness Inventories." European Psychologist 17, no. 3 (January 1, 2012): 222–30. http://dx.doi.org/10.1027/1016-9040/a000097.

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Morningness-eveningness refers to the preference people have regarding the time they like to rise, conduct activities, and go to bed. People denoted as “morning types” (“larks”) like to rise early in the morning and go to bed early, while “evening types” (“owls”) prefer to sleep until later in the day and stay up until later at night. Various self-report instruments that measure morningness-eveningness have been developed. The aim of this study was to validate seven different self-report measures on morningness-eveningness using actigraphic data. One hundred and sixty-six students (mean age 21.4 years, range 19–30) were recruited from the University of Bergen and Bergen University College. The participants completed the self-report measures and wore an actigraph for seven days. The results showed that all self-report measures were in concordance with actigraphy-measured bed times, rise times, and the nadir for physical activity. In addition, some of the instruments were sensitive to differences between morning and evening types in their total sleep time on weekend nights or their stability in the activity curve across days as measured by actigraphy. Both the strengths and weaknesses of the present study are discussed, and proposals for future research are presented.

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50

Sommers, Joseph Michael. "Imagining: An interview with Dave McKean on the early years." Studies in Comics 12, no. 2 (November 1, 2022): 269–78. http://dx.doi.org/10.1386/stic_00072_7.

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Surrounding his early work in art and comics, this 2020 interview conducted with Dave McKean investigates his first years within the comics community with comics luminaries such as Neil Gaiman, Grant Morrison and Karen Berger. In it, McKean reflects on his early years in the world of art, those first meetings with DC Comics alongside Gaiman, and their inculcation into the ‘independent spirit’ of the Vertigo aesthetic and brand. McKean offers direct remark and commentary on his work on books such as The Sandman, Black Orchid and Hellblazer. In the end, even many years later, he still remains somewhat ‘conflicted’ and ‘undecided’ about DC’s editorial department and Karen Berger in her capacities as an editor, or, at least, as his editor.

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