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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Topic

Dronning Maud Land

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Book Section

Results 113 resources

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Abstracts

Engeland, S., & Engeland, S. (2021). Dronning Maud Land: der ingen skulle tru at det var fjell ... In Høyde over havet : hvordan fjellene våre ble målt og satt på kartet (pp. 270–289). Fri flyt AS.
Lundin, K. (2015). Belåtna svenskar i Antarktis. In Pemmikan : en hårdkokt historia (pp. 239–243). Pemmikanförlaget.
Jacobs, J., Läufer, A., Clark, C., Kleinhanns, I., Elburg, M., Ruppel, A., Estrada, S., Damaske, D., Jokat, W., Riedel, S., & Lucka, N. (2013). Neoproterozoic/Lower Palaeozoic geodynamic evolution of Dronning Maud Land: integrating geology and geophysics. In E.-M. Pfeiffer, H. Kassens, M. Scheinert, & R. Tiedemann (Eds.), Changing polar regions : 25th International Congress on Polar Research ; March 17-22, 2013, Hamburg, Germany (Vol. 659, pp. 64–65). Alfred Wegener Institute for Polar and Marine Research. https://doi.org/https://doi.org/10.2312/BzPM_0659_2013

East Antarctica probably formed by amalgamation of a number of cratons along distinct Ediacaran mobile belts, including the ca. 600-500 Ma East African-Antarctic Orogen (EAAO) that dissects Dronning Maud Land (DML). New field-work during the international expeditions Geodynamic Evolution of East Antarctica (GEA) I + II in the austral summers 2010/11 and 2011/12, and first geochronological results from eastern DML reveal a complex tectonic architecture across the belt. In western DML, the EAAO reworks older Mesoproterozoic crust of the Maud Belt; the westernmost boundary of the mobile belt is characterized by a major dextral transpressional shear zone. In central DML, a major magnetic anomaly, the Forster anomaly, was interpreted as a cryptic suture of the EAAO (Riedel et al. 2012). The area where the Forster anomaly crosses the DML mountains is poorly investigated so far, but appears to coincide with a major strike slip shear zone in the southern Kurze Mts. and the occurrence of major Ediacaran granulite bodies. East of the Forster anomaly, the magnetic anomaly pattern changes significantly and typical Maud type crust is not present any longer. GEA II targeted a range of nunataks between Sør Rondane and central DML that had never been visited previously (from Blåklettane and Bergekongen in the E to Urna and Sørsteinen in the W). These nunataks are dominated by medium- to high-grade metasedimentary and metavolcanic rocks of possibly Neoproterozoic age, including abundant marble and graphite schists. Sør Rondane in eastern DML, is dominated by two distinct blocks separated by the dextral Main Shear Zone. The northwestern block is still part of the eastern EAAO, where new SHRIMP zircon data from metamorphic rims provide ages of ca. 560 Ma. The southeastern block is made up of a TTG terrane, which provides four new SHRIMP zircon dates between 990-980 Ma, interpreted as igneous crystallization ages (oceanic arc). The TTG terrane shows limited tectonic overprint and is likely the southeastern foreland of the EAAO. Close to the contact of the two blocks grey geisses and augen-gneisses gave zircon crystallization ages of ca. 750 Ma, ages which were previously unknown from the EAAO. The Forster anomaly therefore separates distinctly different parts of the EAAO: a) a reworked, mainly Grenville-age crust to the W (the overprinted margin of the Kalahari Craton) and b) a part of the orogen dominated by Neoproterozoic accretionary tectonics to the E. This difference is also reflected in the geochemistry of voluminous late-tectonics granitoids across the belt.
Winther, J.-G., & Coulthard, A. (2011). Clues to historical climate variation and future changes in sea level buried in the Antarctic ice (TASTE-IDEA). In O. Orheim & K. Ulstein (Eds.), International Polar Year 2007-2008 : the Norwegian contribution (pp. 88–92). Research Council of Norway.
Winther, J.-G., & Isaksson, E. (2011). Svarene på fortidens klimavariasjoner og framtidens havnivå ligger begravd i isen i Antarktis. In K. Ulstein & O. Orheim (Eds.), Polaråret 2007-2008 : det norske bidraget (pp. 89–92). Norges forskningsråd. https://doi.org/oai:nb.bibsys.no:991122954014702202 URN:NBN:no-nb_digibok_2014120907592

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Engvik, A. K., Elvevold, S., Jacobs, J., Tveten, E., de Azevedo, S., & Njange, F. (2007). Pan-African granulites of central Dronning Maud Land and Mozambique: a comparison within the East-African-Antarctic orogen. In A. Cooper & C. Raymond (Eds.), Antarctica - a keystone in a changing world: online proceedings for the 10th International Symposium on Antarctic Earth Sciences (pp. 1–5). National Academic Press.

Granulite-facies metamorphism is extensively reported in Late Neoproterozoic/Early Palaeozoic time during formation of the East-African-Antarctic orogen (EAAO). Metamorphic data acquired from the Pan-African orogen of central Dronning Maud Land (cDML) are compared with data from northern Mozambique. The metamorphic rocks of cDML are characterised by Opx±Grt-bearing gneisses and Sil+Kfs-bearing metapelites which indicate medium-P granulite-facies metamorphism. Peak conditions, which are estimated to 800-900ºC at pressures up to 1.0 GPa, were followed by near-isothermal decompression during late Pan-African extension and exhumation. Granulite-facies lithologies are widespread in northern Mozambique, and Grt+Cpx-bearing assemblages show that high-P granulitefacies conditions with PT reaching 1.55 GPa and 900ºC were reached during the Pan-African orogeny. Garnet is replaced by symplectites of Pl+Opx+Mag indicating isothermal decompression, and the subsequent formation of Pl+amphibole-coronas suggests cooling into amphibolite facies. It is concluded that high-T metamorphism was pervasive in EAAO in Late Neoproterozoic/Early Paleozoic time, strongly overprinting evidences of earlier metamorphic assemblages.
Engvik, A. K., & Elvevold, S. (2006). Late Pan-African Fluid Infiltration in the Mühlig-Hofmann- and Filchnerfjella of Central Dronning Maud Land, East Antarctica. In D. K. Fütterer, D. Damaske, G. Kleinschmidt, H. Miller, & F. Tessensohn (Eds.), Antarctica: Contributions to Global Earth Sciences. Proceedings of the IX International Symposium of Antarctic Earth Sciences Potsdam, 2003 (pp. 55–62). Springer. https://doi.org/10.1007/3-540-32934-x_7

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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.
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.
Bauer, W., Thomas, R. J., & Jacobs, J. (2003). Proterozoic–Cambrian history of Dronning Maud Land in the context of Gondwana assembly. In M. Yoshida, B. F. Windley, & S. Dasgupta (Eds.), Proterozoic East Gondwana: Supercontinent Assembly and Breakup (Vol. 206, pp. 247–269). Geological Society of London. https://doi.org/10.1144/gsl.Sp.2003.206.01.13

Dronning Maud Land contains a fragment of an Archaean craton covered by sedimentary and magmatic rocks of Mesoproterozoic age, surrounded by a Late Mesoproterozoic metamorphic belt. Tectonothermal events at the end of the Mesoproterozoic and in Late Neoproterozoic–Cambrian times (Pan-African) have been proved within the metamorphic belt. In western Dronning Maud Land a juvenile Mesoproterozoic basement was accreted to the craton at c. 1.1 Ga. Mesoproterozoic rocks were also detected by zircon SHRIMP dating of gneisses in central Dronning Maud Land, followed by a long hiatus for which geochronological data are lacking, an amphibolite to granulite facies metamorphism and syntectonic granitoid emplacement of Pan-African age have been dated. During this orogeny older structures were completely overprinted in a sinistral tranpressive deformation regime, leading to the mainly coast-parallel tectonic structures of the East Antarctic Orogen. Putting Antarctica back in its Gondwana position, the East Antarctic Orogen continues northward in East Africa as the East African Orogen, whereas a connection to the marginal Ross Orogen at the Pacific margin of East Antarctica is suggested along the Shackleton Range. The East Antarctic-East African Orogen resulted from closure of the Mozambique Ocean and collision of West and East Gondwana, i.e. western Dronning Maud Land was part of West Gondwana. During this collision the lithospheric mantle probably delaminated, allowing the asthenosphere to underplate the continental crust and producing heat for the voluminous, typically anhydrous, Pan-African granitoids of central Dronning Maud Land.

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Njåstad, B. (2002). Environmental aspects of the 2000/2001 Norwegian Antarctic research expedition. In J.-G. Winther (Ed.), Norwegian Antarctic Research Expedition (NARE) 2000/2001 (Vol. 120, pp. 11–13). Norsk Polarinstitutt. http://hdl.handle.net/11250/173258

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Nøst, O. A., Goodwin, H., Rønstad, T., & Thorsen, S. H. (2002). Measuring ice shelf draft and seabed topography below Fimbulisen. In J.-G. Winther (Ed.), Norwegian Antarctic Research Expedition (NARE) 2000/2001 (Vol. 120, pp. 30–37). Norsk Polarinstitutt. http://hdl.handle.net/11250/173258

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Tveraa, T., Birkeland, I., Henden, J.-A., & Varpe, Ø. (2002). Studies of population dynamics and life history strategies of Antarctic petrels at Svarthamarehn. In J.-G. Winther (Ed.), Norwegian Antarctic Research Expedition (NARE) 2000/2001 (Vol. 120, pp. 15–17). Norsk Polarinstitutt. http://hdl.handle.net/11250/173258

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Winther, J.-G., Karlöf, L., Hofstede, C., Johansen, E., Johansen, J.-T., De Jong, E.-J., Kaspers, K., Lappegard, G., Pettersson, R., Tronstad, S., & Van De Wal, R. (2002). European project for ice coring in Antarctica (EPICA) - Nordic traverse in 2000/01. In J.-G. Winther (Ed.), Norwegian Antarctic Research Expedition (NARE) 2000/2001 (Vol. 120, pp. 18–29). Norsk Polarinstitutt. http://hdl.handle.net/11250/173258

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Karlöf, L., Gjerde, K., & Winther, J.-G. (1999). EPICA Dronning Maud Land pre-site survey. In T. (ed. ) Tveraa & J.-G. (ed. ) Winther (Eds.), Report of the Norwegian Antarctic Research Expedition 1997/98 (Vol. 156, pp. 8–18). Norsk Polarinstitutt. https://brage.npolar.no/npolar-xmlui/handle/11250/173073

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Tveraa, T., Andreassen, C., & Christensen, G. N. (1999). Studies of seabirds at Svarthamaren. In T. (ed. ) Tveraa & J.-G. (ed. ) Winther (Eds.), Report of the Norwegian Antarctic Research Expedition 1997/98 (Vol. 156, pp. 26–29). Norsk Polarinstitutt. https://brage.npolar.no/npolar-xmlui/handle/11250/173073

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Austrheim, H., Elvevold, S., Engvik, A. K., & Paulsson, O. (1997). Geological observations in Gjelsvikfjella, Mühlig-Hogmanfjella and western Orvinfjella during NARE 96/97. In J.-G. (ed. ) Winther (Ed.), Report of the Norwegian Antarctic Research Expedition 1996/97 (Vol. 148, pp. 77–84). Norsk Polarinstitutt. https://brage.npolar.no/npolar-xmlui/handle/11250/173024

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Barstad, B., Eiken, T., Finnes, R., & Øvstedal, O. (1997). Geodetic measurements in Dronning Maud Land. In J.-G. (ed. ) Winther (Ed.), Report of the Norwegian Antarctic Research Expedition 1996/97 (Vol. 148, pp. 67–75). Norsk Polarinstitutt. https://brage.npolar.no/npolar-xmlui/handle/11250/173024

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Barstad, B., Eiken, T., & Lytskjold, B. (1997). Geodetic and topographic work. In Report of the Norwegian Antarctic Research Expedition 1992/93 (Vol. 125, pp. 74–81). Norsk Polarinstitutt. https://brage.npolar.no/npolar-xmlui/handle/11250/173096

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Falk-Petersen, S., & Lønne, O. J. (1997). Zooplankton in the marginal ice zone off Dronning Maud Land - population structure and trophic relationship. In Report of the Norwegian Antarctic Research Expedition 1992/93 (Vol. 125, pp. 29–36). Norsk Polarinstitutt. https://brage.npolar.no/npolar-xmlui/handle/11250/173096

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