Antarktis-bibliografi er en database over den norske Antarktis-litteraturen.

Hensikten med bibliografien er å synliggjøre norsk antarktisforskning og annen virksomhet/historie i det ekstreme sør. Bibliografien er ikke komplett, spesielt ikke for nyere forskning, men den blir oppdatert.

Norsk er her definert som minst én norsk forfatter, publikasjonssted Norge eller publikasjon som har utspring i norsk forskningsprosjekt.

Antarktis er her definert som alt sør for 60 grader. I tillegg har vi tatt med Bouvetøya.

Det er ingen avgrensing på språk (men det meste av innholdet er på norsk eller engelsk). Eldre norske antarktispublikasjoner (den eldste er fra 1894) er dominert av kvalfangst og ekspedisjoner. I nyere tid er det den internasjonale polarforskninga som dominerer. Bibliografien er tverrfaglig; den dekker både naturvitenskapene, politikk, historie osv. Skjønnlitteratur er også inkludert, men ikke avisartikler eller upublisert materiale.

Til høyre finner du en «HELP-knapp» for informasjon om søkemulighetene i databasen. Mange referanser har lett synlige lenker til fulltekstversjon av det aktuelle dokumentet. For de fleste tidsskriftartiklene er det også lagt inn sammendrag.

Bibliografien er produsert ved Norsk Polarinstitutts bibliotek.

Your search

Topic

Dronning Maud Land

Results 625 resources

1
...
14
15
16
17
18
...
32

Page 16 of 32

Abstracts

Bucher-Nurminen, K., Ohta, Y., Austrheim, H., & Dallmann, W. K. (1990). Geological observations in Gjelsvikfjella and Mühling-Hofmannfjella. In Report of the Norwegian Antarctic Research Expedition 1989/90 (Vol. 113, pp. 91–100). Norsk Polarinstitutt. https://doi.org/oai:nb.bibsys.no:999101870964702202 URN:NBN:no-nb_digibok_2007102600009

View on urn.nb.no
Dallmann, W. K., Austrheim, H., Bucher-Nurminen, K., & Ohta, Y. (1990). Geology around the Norwegian Antarctic station “Troll”, Jutulsessen, Dronning Maud Land (Vol. 111). Norsk Polarinstitutt. https://brage.npolar.no/npolar-xmlui/handle/11250/173018

During the Norwegian Antarctic Research Expedition 1989/90, a pennanent, unmanned research station was raised in Jutulsessen, Gjelsvikfjella, western Dronning Maud Land. The present report is a description of the geology of the area accessable from the station. Exposures of rocks in this part of Dronning Maud Land are restricted to a coastal mountain chain at c. 200-250 km distance from the ice shelf edge at elevations between 1000 and 3000 m. Quaternary deposits are particularly restricted to the inner parts of the Jutulsessen glaeier cirques. Deposits are till and talus which locally are admixing at slope angles of c. 25°. Moraines are poorly developed. Patterned ground ('stone pits') are common at slope angles below c. 15°. Recently active phenomena of special interest are ice-margin meltwater lakes with pingo-like 'blisters " the deep frost-shattering all over the mountain walls and hoIes in rock surfaces as a result of wind activity with grinding particles. The bedrock belongs to the East Antarctic craton. The area under consideration (western Miihlig-Hofmannfjella and Gjelsvikfjella) consists of high-grade metamorphic rocks and fonns one of the world's best exposed granulite terranes. Orthogneisses and minor metasediments have been intruded by a series of charnockites, partly altered to granulites (the 'Svarthamaren charnockite complex'), and a sequence of dyke rocks. Migmatization has affected large parts of the gneisses. Both gneisses and granulites/charnockites show abundant evidence of transition from granulite to amphibolite facies and vice versa, and the important role of fluid-rock interactions leading to these processes can be studied. The gneisses at Jutulsessen show a complex defonnation history. They are thought to be derived from granitic intrusions, though minor amounts of high-grade metamorphic, metapelitic gneisses may represent their original host rocks. Early tectonism (c. 1000-1200 m.y.) produced gneissosity, compositional banding and a leucosome phase under high-grade metamorphic conditions. This was followed by multiple and complex intrusive activity, partial migmatization and a tectonic overprint with abundant shear defonnation under amphibolite-facies conditions (c. 450-500 m.y.).

View on brage.npolar.no
Eiken, T., Luktvasslimo, B. Å., & Lytskjold, B. (1990). Geodetic measurements in Dronning Maud Land. In Report of the Norwegian Antarctic Research Expedition 1989/90 (Vol. 113, pp. 101–112). Norsk Polarinstitutt. https://doi.org/oai:nb.bibsys.no:999101870964702202 URN:NBN:no-nb_digibok_2007102600009

View on urn.nb.no
Imbert, B. C., & Hem, A. (1990). I hjertet av Antarktis; Norge i Antarktis. In Polarforskningens pionerer (Vol. 3, pp. 79–107, 129–134). Schibsted. https://doi.org/oai:nb.bibsys.no:999010468684702202 URN:NBN:no-nb_digibok_2008061004006

View on urn.nb.no
Kennett, M. (1990). Radio-echo investigations in Dronning Maud Land. In Report of the Norwegian Antarctic Research Expedition 1989/90 (Vol. 113, pp. 75–79). Norsk Polarinstitutt. https://doi.org/oai:nb.bibsys.no:999101870964702202 URN:NBN:no-nb_digibok_2007102600009

View on urn.nb.no
Molvær, O. I., Bendiksen, F. S., & Reitehaug, P.-I. (1990). Medical contingency and biomedical research. In Report of the Norwegian Antarctic Research Expedition 1989/90 (Vol. 113, pp. 113–123). Norsk Polarinstitutt. https://doi.org/oai:nb.bibsys.no:999101870964702202 URN:NBN:no-nb_digibok_2007102600009

View on urn.nb.no
Norsk, P. (1990). Report of the Norwegian Antarctic Research Expedition 1989/90 (O. Orheim, Ed.; Vol. 113). Norsk Polarinstitutt. https://doi.org/oai:nb.bibsys.no:999101870964702202 URN:NBN:no-nb_digibok_2007102600009

View on urn.nb.no
Ohta, Y., Tørudbakken, B., & Shiraishi, K. (1990). Geology of Gjelsvikfjella and western Mühlig-Hofmannfjella, Dronning Maud Land, east Antarctica. Polar Research, 8(2), 99–126. https://doi.org/10.3402/polar.v8i2.6808

As a part of the Norwegian Antarctic Research Expedition 1984/85, geological mapping was performed in Gjelsvikfjella and western Muhlig-Hofmannfjella, Dronning Maud Land. The northern part of Gjelsvikfjella is dominated by the Jutulsessen metasupracrustals which have been intruded by a major gabbroic body and several generations of dykes. To the south the metasupracrustals gradually transform into the Risemedet migmatites. In western Muhlig-Hofmannfjella the bedrock is dominated by the large Svarthamaren Charnockite batholith. The batholith is bordered by the Snotoa metamorphic complex outcropping to the south and west in Muhlig-Hofmannfjella and it is characterized by a high content of partly assimilated country rock inclusions. Mineral paragenesis and geothermometry/geobarometry suggest a two-stage tectonothermal-igneous history with an initial intermediate pressure, upper amphibolite to granulite facies metamorphism followed by high temperature transformations related to the charnockite intrusion. The age of the initial tectonothermal event is probably about 1,100 Ma. Geochronological work in the present study (Rb/Sr whole rock) gave an age of 500 +/- 24 Ma for the Svarthamaren Charnockite, interpreted to record the age of crystallization. Late brittle faulting and undeformed dolerite dykes outcropping in Jutulsessen are believed to be related to Mesozoic crustal stretching in the Jutulstraumen-Pencksokket Rift Zone to the west.

View on polarresearch.net
Orheim, O., Hagen, J. O., Østerhus, S., & Sætrang, A. (1990). Glaciologic and oceanographic studies on Fimbulisen during NARE 1989/90. Filchner-Ronne Ice Shelf Programme. Report, 4, 120–131.
Orheim, O., Hagen, J. O., Østerhus, S., & Sætrang, A. (1990). Studies on, and underneath, the Ice Shelf Fimbulisen. In Report of the Norwegian Antarctic Research Expedition 1989/90 (Vol. 113, pp. 59–73). Norsk Polarinstitutt. https://doi.org/oai:nb.bibsys.no:999101870964702202 URN:NBN:no-nb_digibok_2007102600009

View on urn.nb.no
Orheim, O., & Lucchitta, B. (1990). Investigating Climate Change by Digital Analysis of Blue Ice Extent on Satellite Images of Antarctica. Annals of Glaciology, 14, 211–215. https://doi.org/10.3189/S0260305500008600
Orheim, O., & Luchitta, B. (1990). lnvestigating climate change by digital analysis of satellite imagery of blue ice extent in Antarctica. Annals of Glaciology, 14, 211–215. https://doi.org/10.3189/S0260305500008600

Landsat-5 Thematic Mapper (TM) and SPOT data collected two years apart from an identical area of Dronning (Queen) Maud Land, Antarctica, have been analyzed to detect variations in surface features that may signal climatic change, and to establish a technique that readily identifies such changes. We found that selective principal component analysis (Chavez and Kwarteng 1989), on band ratios of near-IR/green, highlights changes in blue ice areas. The formation and preservation of blue ice is poorly understood, but we suggest that it generally takes longer to increase a blue ice area than to decrease it, and that blue ice extent is most sensitive to changes in accumulation rate. The investigated blue ice area shows a decrease in extent over the two-year period caused by incursion of snow that probably resulted from an increase in accumulation rate. Comparison of two TM images collected 18 days apart shows that transitory snow drifts have little effect on blue ice extent.
Pedersen, H. C. (1990). Aspects of reproductive behaviour in a population of South Polar skua Catharacta maccormicki in Dronning Maud Land. In Report of the Norwegian Antarctic Research Expedition 1989/90 (Vol. 113, pp. 43–45). Norsk Polarinstitutt. https://doi.org/oai:nb.bibsys.no:999101870964702202 URN:NBN:no-nb_digibok_2007102600009

View on urn.nb.no
Røv, N. (1990). Studies of breeding biology of Antarctic petrel and snow petrel in Mühlig-Hofmannfjella, Dronning Maud Land. In Report of the Norwegian Antarctic Research Expedition 1989/90 (Vol. 113, pp. 47–51). Norsk Polarinstitutt. https://doi.org/oai:nb.bibsys.no:999101870964702202 URN:NBN:no-nb_digibok_2007102600009

View on urn.nb.no
Strømme, A. (1990). Ecophysiological adaptations in mites and collembolans in Dronning Maud Land. In Report of the Norwegian Antarctic Research Expedition 1989/90 (Vol. 113, pp. 53–57). Norsk Polarinstitutt. https://doi.org/oai:nb.bibsys.no:999101870964702202 URN:NBN:no-nb_digibok_2007102600009

View on urn.nb.no
Sunding, P. (1990). Bibliographia Phytosociologica. Norwegian possessions in the polar regions. Excerpta botanica, Sectio B, 27, 157–169.
Sæther, B.-E., Andersen, R., & Pedersen, H. C. (1990). Studies on the factors determining variation in the reproductive success of the Antarctic petrel Thalassoica antarctica in Svarthamaren, Mühlig-Hofmannfjella. In Report of the Norwegian Antarctic Research Expedition 1989/90 (Vol. 113, pp. 37–41). Norsk Polarinstitutt. https://doi.org/oai:nb.bibsys.no:999101870964702202 URN:NBN:no-nb_digibok_2007102600009

View on urn.nb.no
Winther, J.-G. (1990). Glaciological and meteorological measurements in Dronning Maud Land. In Report of the Norwegian Antarctic Research Expedition 1989/90 (Vol. 113, pp. 81–86). Norsk Polarinstitutt. https://doi.org/oai:nb.bibsys.no:999101870964702202 URN:NBN:no-nb_digibok_2007102600009

View on urn.nb.no
Amlien, J. (1989). Satellittkartlegging ved Norsk Polarinstitutt. Kart og plan, 49(6), 519–522. https://doi.org/oai:urn.nb.no:no-nb_digitidsskrift_2013061382042_001 URN:NBN:no-nb_digitidsskrift_2013061382042_001

View on urn.nb.no
Friberg, F. (1989, desember). Miljøspørsmål i fokus: forskningsskipet “Andenes” på vei mot Antarktis. Svalbardposten, 8, 10–11. https://urn.nb.no/URN:NBN:no-nb_digavis_svalbardposten_null_null_19891220_41_50_1

View on urn.nb.no

1
...
14
15
16
17
18
...
32

Page 16 of 32

Last update from database: 3/1/25, 3:17 AM (UTC)