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.

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Publication year

Between 2000 and 2025
- Between 2000 and 2009
  - 2004

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Results 18 resources

Abstracts

Barr, S. (2004). Ekspedisjoner og begivenheter. In E.-A. Drivenes & H. D. Jølle (Eds.), Norsk polarhistorie: Vol. 1 : Ekspedisjonene (pp. 411–421). Gyldendal.
Barr, S. (red. ), & Chaplin, P. (red. ). (2004). Cultural heritage in the Arctic and Antarctic regions (Vol. 8). ICOMOS International Polar Heritage Committee.
Basberg, B. L. (2004). Whalers, explorers and scientists: historical perspectives on the development of the antarctic whaling industry. In A. Elzinga, T. Nordin, D. Turner, & U. Wråkberg (Eds.), Antarctic challenges : historical and current perspectives on Otto Nordenskjöld’s Antarctic expedition 1901-1903 (Vol. 5, pp. 25–38). Royal Society of Arts and Sciences.
Berg, R. (2004). Amundsen og hans aeronauter. In E.-A. Drivenes & H. D. Jølle (Eds.), Norsk polarhistorie: Vol. 1 : Ekspedisjonene (pp. 279–286). Gyldendal.
Elstad, Å. (2004). Den første norske oljealderen. In E.-A. Drivenes & H. D. Jølle (Eds.), Norsk polarhistorie: Vol. 3 : Rikdommene (pp. 275-[315]). Gyldendal.
Elstad, Å. (2004). Polarturisme. In E.-A. Drivenes & H. D. Jølle (Eds.), Norsk polarhistorie: Vol. 3 : Rikdommene (pp. 477-[519]). Gyldendal.
Elstad, Å., & Finstad, B.-P. (2004). Ein grådig fangstnasjon? In E.-A. Drivenes & H. D. Jølle (Eds.), Norsk polarhistorie: Vol. 3 : Rikdommene (pp. 319-[387]). Gyldendal.
Engvik, A. K., & Elvevold, S. (2004). Pan-African extension and near-isothermal exhumation of a granulite facies terrain, Dronning Maud Land, Antarctica. Geological Magazine, 141(6), 649–660. https://doi.org/10.1017/S0016756804009859

The Mühlig-Hofmann- and Filchnerfjella in central Dronning Maud Land, Antarctica, consist of series of granitoid igneous rocks emplaced in granulite and upper amphibolite facies metamorphic rocks. The area has experienced high-temperature metamorphism followed by near-isothermal decompression, partial crustal melting, voluminous magmatism and extensional exhumation during the later phase of the late Neoproterozoic to Cambrian Pan-African event. Remnants of kyanite–garnet–ferritschermakite–rutile assemblages indicate an early higher-pressure metamorphism and crustal overthickening. The gneisses experienced peak granulite facies temperatures of 800–900 °C at intermediate pressures. Breakdown of garnet + sillimanite + spinel-bearing assemblages to cordierite shows subsequent re-equilibration to lower pressures. An E–W foliation dominating the gneisses illustrates transposition of migmatites and leucocratic melts which evolved during the near-isothermal decompression. Occurrence of extensional shear bands and shear zones evolving from the ductile partial melting stage through semiductile towards brittle conditions, shows that the uplift persisted towards brittle crustal conditions under tectonic W/SW-vergent extension. Late-orogenic Pan-African quartz syenites intruded after formation of the main gneiss fabric contain narrow semiductile to brittle shear zones, illustrating that the extensional exhumation continued also after their emplacement. The latest record of the Pan-African event is late-magmatic fluid infiltration around 350–400 °C and 2 kbar. At this stage the Pan-African crust had undergone 15–20 km exhumation from the peak granulite facies conditions. We conclude that the later phase of the Pan-African event in central Dronning Maud Land is characterized by a near-isothermal decompression P–T path and extensional structures indicating tectonic exhumation, which is most likely related to a late-orogenic collapsing phase of the Pan-African orogen.
Eriksen, A. (2004). Polarheltene - minner og monumenter. In E.-A. Drivenes & H. D. Jølle (Eds.), Norsk polarhistorie: Vol. 1 : Ekspedisjonene (pp. 345–388). Gyldendal.
Fleming, F. (2004). The race for the South Pole: Robert Scott and Roald Amundsen (1911-12). In Off the map : tales of endurance and exploration (pp. 422–431). Grove Press.
Friedman, R. M. (2004). Å spise kirsebær med de store. In E.-A. Drivenes & H. D. Jølle (Eds.), Norsk polarhistorie: Vol. 2 : Vitenskapene (pp. 331-[419]). Gyldendal.
Fulsås, N. (2004). En æressag for vor nation. In E.-A. Drivenes & H. D. Jølle (Eds.), Norsk polarhistorie: Vol. 1 : Ekspedisjonene (pp. 209–220). Gyldendal.
Goksøyr, M. (2004). Kappløp i gamle spor. In E.-A. Drivenes & H. D. Jølle (Eds.), Norsk polarhistorie: Vol. 1 : Ekspedisjonene (pp. 305–342). Gyldendal.
Hessen, D. O. (2004). Klodens helse - sett fra polene. In E.-A. Drivenes & H. D. Jølle (Eds.), Norsk polarhistorie: Vol. 2 : Vitenskapene (pp. 474–490). Gyldendal.
Hofstede, C. M., Roderik, S. W. van de W., Kaspers, K. A., van den Broeke, M. R., Karlöf, L., Winther, J.-G., Isaksson, E., Lappegard, G., Mulvaney, R., Oerter, H., & Wilhelms, F. (2004). Firn accumulation records for the past 1000 years on the basis of dielectric profiling of six cores from Dronning Maud Land, Antarctica. Journal of Glaciology, 50(169), 279–291. https://doi.org/10.3189/172756504781830169

This paper presents an overview of firn accumulation in Dronning Maud Land (DML), Antarctica, over the past 1000 years. It is based on a chronology established with dated volcanogenic horizons detected by dielectric profiling of six medium-length firn cores. In 1998 the British Antarctic Survey retrieved a medium-length firn core from western DML. During the Nordic EPICA (European Project for Ice Coring in Antarctica) traverse of 2000/01, a 160 m long firn core was drilled in eastern DML. Together with previously published data from four other medium-length ice cores from the area, these cores yield 50 possible volcanogenic horizons. All six firn cores cover a mutual time record until the 29th eruption. This overlapping period represents a period of approximately 1000 years, with mean values ranging between 43 and 71 mm w.e. The cores revealed no significant trend in snow accumulation. Running averages over 50 years, averaged over the six cores, indicate temporal variations of5%. All cores display evidence of a minimum in the mean annual firn accumulation rate around AD 1500 and maxima around AD 1400 and 1800. The mean increase over the early 20th century was the strongest increase, but the absolute accumulation rate was not much higher than around AD 1400. In eastern DML a 13% increase is observed for the second half of the 20th century.
Nielsen, S. H. H. (2004). Southern Ocean climate variability. University of Tromsø and Norwegian Polar Institute.
Næss, A. (2004). De tre store. In E.-A. Drivenes & H. D. Jølle (Eds.), Norsk polarhistorie: Vol. 1 : Ekspedisjonene (pp. 136–165). Gyldendal.
Smedsrud, L. H. (Ed.). (2004). 17th International FRISP Workshop held at the British Antarctic Survey, Cambridge, U.K. on 17th and 18th June 2003 (Vol. 15). Bjerknes Centre for Climate Research.

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