Oslo region

Baarli, B.G. and Johnson, M.E. (1988) Biostratigraphy of key brachiopod lineages from the Llandovery Series (Lower Silurian) of the Oslo Region. Norsk Geologisk Tidsskrift, 68, 259-274. 

St. Joseph, J.K.S. (1938) The Pentameracea of the Oslo region being a description of the Kiaer collection of pentamerids. Norsk Geologisk Tidsskrift, 17, 225-336. 

The Ordovician rocks of the eastern-most part of the Baltic palaeocontinent were deposited in a remarkable epicontinental basin with no apparent modern analogues. Sediment rates were very low, in the order of 1-3 mm per 1,000 years and predominantly carbonates. The seafloor had little topography and the eastern part of the basin, at least, was tectonically stable for much of its history. Carbonate sediments were generated across much of the continent during most of the period. In the East Baltic the Ordovician succession reaches a thickness of up to 250 m in the central part of the region, in west Latvia. To the west, however, in the Oslo Region, thicker successions, in the order of 1.5 km, are characterised by the significant input of siliciclastic material from the adjacent Caledonian mountain belt (Bruton and Harper, 1988). 

Figure 32.4 Taxonomic profiles through the Central Oslo Region succession. The local diversity of taxa is indicated as numbers of genera. The sequence template of Dronov and Holmer (1990) for Baltoscandia is indicated on the right and the position of the main bentonite is marked by asterisks.

Harper, D.A.T. (1986) Distributional trends within the Ordovician brachiopod faunas of the Oslo Region, south Norway. Biostratigraphie du Paleozoique, 4, 465M75. 

Bjorlykke K. Depositional history and geochemical composition of Lower Palaeozoic epicontinental sediments from the Oslo region. Norg. geol. Unders. no. 305, 1974, 81 p. 

Bowring, R. W., 1962, Physical Model, Based on Bubble Detachment and Calculation of Steam Voi-dage in the Subcooled Region of a Heated Channel, Inst, for Atomenergie Rep. HRP-10, Oslo, Norway. (3)... 

During regional scale ozone episodes, elevated concentrations become widespread across Europe [20]. Transboundary transport is an important feature of the problem. The concentrations exceed air quality guidelines set to protect human health [22] and critical levels set to protect crops and trees firom ozone damage. To illustrate the approach, the target ecosystem is taken to be human health so that the sensitive ecosystems can be located in the major urban centres of London, Paris, Brussels, Bonn, Amsterdam, Copenhagen, Stockholm and Oslo. For these ecosystems, the maximum hourly mean in a worst-case episode is the most appropriate index of harm. 

In Norway, the non-hydrostatic MM5 model (Grell et al., 1994 [234]) is nested with the HIRLAM NWP model (Berge et al., 2002 [58]). The latter model is operated on a 10 km horizontal resolution for North-Western Europe. A domain with a resolution of 3 km has been set up for the region around the city of Oslo in which MM5 is one-way nested with HIRLAM. A two-way nesting takes place between the 3 km resolution... 

The pure fluidized bed crystallizers described later in Example 7-6, while designed for a particular purpose, have many similarities with the Oslo commercial surface-cooled crystallizer shown in Fig. 7-10. A fluidized magma in the crystallizer body (E) carries out the crystallization. Feed enters the clear overflow stream (at G), is cooled within the metastable super-saturation region in the cooler (H), and then enters as a fluidizing stream at the bottom of (E). 

Weller, G. and Lange, M. (1999) Impacts of Global Climate Change in the Arctic Regions. An Initial Assessment, International Arctic Science Committee (IASC), Oslo, Norway. 

Xu, B. 2003. Biodegradation and accumulation of oils and condensates in the Donna Region—Norwegian Offshore Continental Shelf (NOCS), Cand. Scient. thesis. Department of Geology, University of Oslo. 

Despite the measures that were taken to control SO and NO, emissions in the first generation of protocols, scientific evidence showed that large parts of Europe were still under threat of acid rain damage and that there were far more ecologically sensitive regions than had been first understood. Eurther measures would have to be taken to reduce harmful emissions. This led to the negotiations for the 1994 Oslo Protocol. The Oslo Protocol essen-... 

Fig. 5. Piincijjal component analysis scores scatter plot of the FTIR data set in the spectral window of 3000-600 cnri wavenumber (1700 data points) of propolis samples produced in the southern Brazil (Santa Catarina State). NRi, NR2 and HL refer to propolis samples originated from northern and highland regions of Santa Catarina State. The calculations were carried out using The Unscrambler software (v. 9.1, Oslo - Norway). PCI and PC2 accoimts for 88% of the variance preserved.

ASSOCIATION "BELLUNA" S REPORT, "Radioactive Contamination Causes in Murmansk and Arkhangelsk Regions", (Boks 8874, Youngstorget N-0028, Oslo, Norway, Version 1,1994). 

Fig. 1.18 Roeild Amundsen of Norway was not a man who smiled a lot. He was instead driven by his passion for exploration of the polar regions. Being a thorough and methodical person, he trained himself and his companions in the art of polar travel and planned meticulously in order to assure success without injury to the members of his team. This portrait of Amundsen is displayed in Oslo in the museum that houses the Pram, the ship in which he and his men traveled to Antarctica for the purpose of reaching the South Pole...

Scenario Damage to culvert The main event selected for illustration in this paper is Damage to culvert/joint conduit of electric power, ICT, and water mains . This event is based on an actual event that occurred in Oslo on November 27th, 2007 An entrepreneur unwarily broke a cable when digging a ditch, and the cable break led to short circuit and fire at the Oslo S railway station (Oslo Central Station), further paralyzing the region s rail traffic and transportation systems for 20 hours, and the internet systems for about 10 hours (DSB 2008). 

Strand, L. (1980). Acid precipitation and regional tree ring analyses SNSF Project, Report IR 73/80, Oslo. 

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