Growth and population parameters of ringed seals (Pusa hispida) from Svalbard, Norway, 2002-2004     

Krafft  Bjorn A.; Kovacs  Kit M.; Frie  Anne Kirstine; Haug  Tore; Lydersen  Christian 《ICES Journal of Marine Science》2006,63(6):1136-1144

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Seasonal distribution, exploitation and present abundance of stocks of large baleen whales (Mysticeti) and sperm whales (Physeter macrocephalus) in Norwegian and adjacent waters   总被引：1，自引：0，他引：1  

Christensen  Ivar; Haug  Tore; Oien  Nils 《ICES Journal of Marine Science》1992,49(3):341-355

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Predation on herring, Clupea harengus, by minke whales, Balaenoptera acutorostrata, in the Barents Sea     

Lindstrom  Ulf; Haug  Tore; Rottingen  Ingolf 《ICES Journal of Marine Science》2002,59(1):58-70

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Growth, reproductive cycle, and movement of berried European lobsters (Homarus gammarus) in a local stock off southwestern Norway     

Agnalt  Ann-Lisbeth; Kristiansen  Tore S.; Jorstad  Knut E. 《ICES Journal of Marine Science》2007,64(2):288-297

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Trends in age-at-maturity and growth parameters of female Northeast Atlantic harp seals, Pagophilus groenlandicus (Erxleben, 1777)     

Kirstine Frie  Anne; Potelov  Vladimir A; Kingsley  Michael C.S; Haug  Tore 《ICES Journal of Marine Science》2003,60(5):1018-1032

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Cenozoic alongslope processes and sedimentation on the NW European Atlantic margin     

Jan Sverre Laberg  Martyn S. Stoker  K.I. Torbjrn Dahlgren  Henk de Haas  Haflidi Haflidason  Berit O. Hjelstuen  Tove Nielsen  Pat M. Shannon  Tore O. Vorren  Tjeerd C.E. van Weering  Silvia Ceramicola 《Marine and Petroleum Geology》2005,22(9-10):1069

Based on studies of sediment accumulations deposited from-and erode by-alongslope flowing ocean currents on the European continental margin from Porcupine (Ireland) to Lofoten (Norway), the evolution of the Cenozoic paleocirculation was reconstructed as part of the STRATAGEM project. There is evidence of ocean current-controlled erosion and deposition in the Rockall Trough, in the Faeroe-Shetland Channel and on the Vøring Plateau since the late Eocene, although the circulation pattern remains ambiguous. The late Palaeogene flow in the Rockall Trough was almost probably driven by southerly-derived Tethyan Outflow Water. The extent and strength of any northerly-derived flow is uncertain. From the early Neogene (early-mid-Miocene), there was a massive regional expansion of contourite drift development both in the North Atlantic and in the Norwegian-Greenland Sea. This was most probably related to the development of the Faroe Conduit, the opening of the Fram Strait and the general subsidence of the Greenland-Scotland Ridge. These may have combined to cause a considerable acceleration in the exchange and overflow of deep waters between the Arctic and Atlantic Oceans. An early late Neogene (late early Pliocene) regional erosional event has been ascribed to a vigorous pulse of bottom-current activity, most probably the result of a global reorganisation of ocean currents associated with the closure of the Central American Seaway. During the late Neogene, contourites and sediment drifts developed in deep-water basins, between units of glacigenic sediments as well as infill of several paleo-slide scars. These sediments were derived from areas of bottom-current erosion as well as from the development of Plio-Pleistocene prograding sediment wedges, incorporating the extensive sediment supply derived from shelf-wide ice sheets. Presently a profound winnowing prevails along the shelf and upper slope due to the inflowing currents of Atlantic water. Depocentres of sediments derived from the winnowing are located (locally) in lower slope embayments and in slide scars.  相似文献   

Basic volcanic rocks and tectonic setting. A discussion of the Zr-Ti-Y discrimination diagram and its suitability for classification purposes     

Tore Prestvik 《Lithos》1982,15(3):241-247

The Zr-Ti-Y diagram cannot discriminate between normal and anomalous oceanic ridge basalts: the latter tend to plot as within-plate basalts. This indicates that it is the mantle anomaly rather than the tectonic setting that characterizes the Zr-Ti-Y interelement ratios in such rocks. It is shown that rocks with SiO₂<56 of a tholeiitic series indicate a differentiation trend from ocean-floor via within-plate to calc-alkaline basalts. This feature shows that great care should be taken when data for altered or metamorphic rocks are selected for classification by this method.  相似文献   

Pervasive assimilation of carbonate and silicate rocks in the Hortavær igneous complex, north-central Norway     

Calvin G. Barnes  Tore Prestvik  Bjrn Sundvoll  Denny Surratt 《Lithos》2005,80(1-4):179-199

The intrusive complex at Hortavær represents a magma transfer zone in which multiple pulses of gabbroic and dioritic magmas evolved along Fe- and alkali-enrichment trends. Extreme alkali enrichment resulted in nepheline-normative and sparse nepheline-bearing monzodioritic and monzonitic rocks. More evolved monzonitic and syenitic rocks are silica saturated and, in some cases, quartz bearing. Previous and current research recognized an abundance of clinopyroxene and other Ca-rich phases, such as scapolite, grossular-rich garnet, and igneous-textured calcite among the mafic and intermediate rocks. Even the most pyroxene-rich samples contain low Sc concentrations, which suggests early, intense fractionation of clinopyroxene. These features and the alkali enrichment are consistent with assimilation of carbonate-rich host rocks. Carbon isotope ratios of the igneous-textured calcite indicate an origin of the carbon from host rocks rich in calcite, consistent with assimilation. However, low _Nd values (−3.4 to −10.2) and moderate initial ⁸⁷Sr/⁸⁶Sr values (0.7052 to 0.7099) indicate the need for assimilation of quartzofeldspathic rocks as well. Models of combined assimilation and fractional crystallization indicate that assimilation of simple end members, either carbonate or silicate, cannot explain the entire data set. Instead, variable proportions of carbonate and silicate materials were assimilated, with the most pronounced assimilation effects in the mafic rocks. The reasons for variable degrees of assimilation are, as yet, uncertain. It is possible that assimilation of calc-silicate rocks with variable carbonate/silicate proportions resulted in the range of observed compositions. However, the importance of carbonate assimilation in mafic rocks compared to felsic ones suggests that assimilation of carbonates was predominant at high temperature and/or mafic magma compositions and assimilation of silicates was predominant at lower temperature and/or felsic magma compositions. We suggest that the ability of the mafic magma to dissolve higher proportions of carbonate contaminants is the result of the magma's ability to form clinopyroxene as a product of assimilation. In any case, extensive carbonate assimilation was possible because CO₂ escaped from the system.  相似文献   

Comment on Special Issue on Geostatistics with Guest Editor A. G. Journel     

Kyrre Bratvedt  Erik Bølviken  Tore Gimse  Helge Holden  Lars Holden  Ragnar Knarud 《Mathematical Geology》1998,30(2):245-246

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Deglaciation history and post-glacial mass movements in Balsfjord, northern Norway     

Matthias Forwick  Tore O. Vorren 《Polar research》2002,21(2):259-266

The deglaciation history of Balsfjord, northern Norway, and post-glacial mass movement events were investigated. Radiocarbon dates indicate that the Balsfjord glacier retreated from the Tromsø–Lyngen moraines about 10.4 ¹⁴C Ky BP. Between ca. 10.3 ¹⁴C Ky BP and 9.9 ¹⁴C Ky BP, deposition of a distinct end moraine–the Skjevelnes moraine–in the central part of Balsfjord occurred. The transition from glacimarine to open marine sedimentary environment took place before 9.6 ¹⁴C Ky BP. Between ca. 9.5 ¹⁴C Ky BP and 8.4 ¹⁴C Ky BP, at least one local and three regional mass movement events occurred. After this period, no gravity flow activity is preserved in the cores. The high frequency of mass movements in the early post-glacial period is presumed to be due to fast sea level changes and/or tectonic activity induced by rapid isostatic uplift.  相似文献