Chapter 59 Neoproterozoic glaciation of South Norway: from continental interior to rift and pericratonic basins in western Baltica - Photograph supplement

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dc.contributor.authorNystuen, Johan P.
dc.date.accessioned2016-01-04T18:49:15Z
dc.date.available2016-01-04T18:49:15Z
dc.date.issued2011
dc.degree.departmentSchool of Environmental Sciencesen
dc.description.abstractCompanion photographs to the book chapter Nystuen, Johan P. and Lamminen, Jarkko T. 2011. “Neoproterozoic glaciation of South Norway: from continental interior to rift and pericratonic basins in western Baltica.” In: Arnaud, E., Halverson, G. P. and Shields-Zhou, G. (eds) The Geological Record of Neoproterozoic Glaciations. Geological Society, London, Memoirs, 36, 613-622.en_US
dc.identifier.urihttp://hdl.handle.net/10214/9437
dc.language.isoenen_US
dc.rightsAttribution-NonCommercial-NoDerivs 2.5 Canada*
dc.rights.holderThe copyright of the photo rests with the author(s) of the chapter or, where stated, the person who took the photo.
dc.rights.urihttps://creativecommons.org/licenses/by-nc-nd/2.5/ca/*
dc.subjectNeoproterozoicen_US
dc.subjectNeoproterozoic glaciationen_US
dc.subjectSouth Norwayen_US
dc.subjectrift basinen_US
dc.subjectpericratonic basinen_US
dc.subjectBalticaen_US
dc.subjectcontinental interioren_US
dc.titleChapter 59 Neoproterozoic glaciation of South Norway: from continental interior to rift and pericratonic basins in western Baltica - Photograph supplementen_US
dc.typeImageen
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Outcrop of typical diamictite lithology of the Moelv Formation, Bruvollhagan, Moelv. Largest clast of gneiss in the foreground is 1.5 m in diameter. The diamictite is interpreted as formed as a basal till (Photo credit: Johan Petter Nystuen).
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Detail of diamictite of the Moelv Formation, Bruvollhagan, Moelv. Clasts are granite, gneiss, vein quartz, quartzite and limestone (dark grey) (Photo credit: Johan Petter Nystuen).
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Calacarous sandstone of the Biri Formation, interpreted to represent a mixed carbonate-silisiclastic platform deposit, located directly below the glacial Moelv Formation. Road section Øvre Rendal – Hanestad (Photo credit: Johan Petter Nystuen).
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