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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geologi

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Abstracts

Elverhøi, A., & Maisey, G. (1983). Geology and petrology of the Yamato Mountains (R. L. Oliver, P. R. James, & J. B. Jago, Eds.). Cambridge University Press.
Elverhøi, A., & Maisey, G. (1983). Glacial erosion and morphology of the eastern and southeastern Weddell Sea shelf (R. L. Oliver, P. R. James, & J. B. Jago, Eds.). Cambridge University Press.
Gjelsvik, T. (1983). The mineral resources of Antarctica: progress in their identification. In F. Orrego-Vicuna (Ed.), Antarctic Resources Policy: Scientific, Legal and Political Issues (pp. 61–76). Cambridge University Press. https://doi.org/10.1017/CBO9780511735462.004

The increment in informationCareful geological investigations started at a few places in Antarctica after World War II, but gained momentum and became systematic only when the International Geophysical Year started, and when SCAR and its Working Group on Geology were established just 25 years ago. Although geology was not initially part of the IGY programme, it soon became one of the thriving sciences in Antarctica.The growth of Antarctic geosciences can be shown in many ways, for example by the expansion of the Symposium volumes from the first one in 1963, containing 76 papers, to the latest one in August 1982, with 191 papers.The investigations have largely had the character of regional reconnaissance surveys, and the observations have mostly been published as general descriptions with maps at the scale of 1:1 million or smaller. Only one Antarctic nation has a systematic mapping programme of larger scales (1:500,000). In a few cases, such as in areas around some larger stations, more detailed work has been going on, in some cases also related to mineral occurrences. A few programmes are under way that have aspects of being resource-oriented: investigations of the Dufek Massif, a layered intrusion similar to the Cr-, Pt- and Ni-rich Bushfeld complex in South Africa, and sampling of manganese nodules during marine geological surveys. Airborne radiometric surveys and also some marine seismic surveys conducted by national oil companies or by resource-oriented state agencies belong to this category.
Fossum, B. A., Maisey, G. H., & Torsen, H. O. (1982). Marine geophysical research in the Weddell Sea during the Norwegian Antarctic research expedition of 1976-77. In Craddock, Campbell (Ed.), Antarctic geoscience : Symposium on Antarctic Geology and Geophysics, Madison, Wisconsin, U.S.A., August 22-27, 1977: Vol. Series B-Number 4 (pp. 397–405). The University of Wisconsin Press Madison.
Furnes, H., Neumann, E.-R., & Sundvoll, B. (1982). Petrology and geochemistry of Jurassic basalt dykes from Vestfjella, Dronning Maud Land, Antarctica. Lithos, 15(4), 295–304. https://doi.org/https://doi.org/10.1016/0024-4937(82)90020-2

Mineral and whole rocks analyses of 12 Jurassic basalt dykes from Vestfjella, Dronning Maud Land, Antarctica, are presented, and their genesis discussed. On the basis of major oxides and norms the basalts may be classified as olivine and quartz tholeiites. Plotted in the Plag Cpx (Opx + 4Q) and Ol Plag Q projections, the compositions are most compatible with fractional crystallization of olivine, clinopyroxene and plagioclase from a basalt liquid at very low pressure. The ratios between strongly incompatible elements such as Rb, Cs, Zr, Hf, Ta and Th vary considerably, and petrographic mixing calculations give poor fits with respect to Rb, Cs, Ta, Th and light REE. Initial 87Sr/86 Sr ratios range between 0.70347 and 0.70687, and show no correlation with Rb/Sr or any other SIE ratios. The trace element and Sr isotope data thus do not suggest any simple cogenetic petrogenetic model. It is concluded that the basalt melts most plausibly have been contaminated by, or mixed with anatectic melts of crustal material, rather than reflecting mantle heterogeneity.

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Hinz, K., & Krause, W. (1982). The Continental Margin of Queen Maud Land/Antarctica: Seismic Sequences, Structural Elements and Geological Development. Geologisches Jahrbuch. Reihe E, Geophysik, 23, 14–41.
Hjelle, Audun, Ohta, Yoshihide, & Winsnes, Thore S. (1982). Geology and petrology of the Southern Heritage Range, Ellsworth Mountains. In Craddock, Campbell (Ed.), Antarctic geoscience: Vol. Series B-Number 4 (pp. 599–608). The University of Wisconsin Press.
Prestvik, T. (1982). Basic volcanic rocks and tectonic setting. A discussion of the Zr-Ti-Y discrimination diagram and its suitability for classification purposes. Lithos, 15(3), 241–247. https://doi.org/https://doi.org/10.1016/0024-4937(82)90015-9

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Prestvik, T. (1982). The geology, volcanic activity, and age of Bouvetøya, South Atlantic. In Norwegian Antarctic Research Expeditions (1978/79) (Vol. 58, pp. 115–123, ill.).
Prestvik, T. (1982). Trace element geochemistry of volcanic rocks from Bouvetøya, South Atlantic. In Craddock, Campbell (Ed.), Antarctic geoscience: Vol. Series B-Number 4 (pp. 771–774). The University of Wisconsin Press Madison.
Johnson, G. L., Vanney, J.-R., Elverhøi, A., & LaBrecque, J. L. (1981). Morphology of the Weddell Sea and southwest Indian Ocean. Deutsche Hydrografische Zeitschrift, 34(6), 263–272. https://doi.org/10.1007/BF02226642

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Lien, R. (1981). Sea bed feauters in the Blåenga area, Weddell Sea, Antarctica. Université Laval.
Orheim, O., & Elverhøi, A. (1981). Model for submarine glacial deposition. Annals of Glaciology, 2, 123–128. https://doi.org/10.3189/172756481794352135
Prestvik, T., & Winsnes, T. S. (1981). Geology of Bouvetøya, South Atlantic. In Bouvetøya, South Atlantic Ocean : results from the Norwegian Antarctic Research Expeditions 1976/77 and 1978/79 (Vol. 175, pp. 41–69). Norsk Polarinstitutt. https://brage.npolar.no/npolar-xmlui/handle/11250/173650

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Løvlie, R. (1979). Mesozoic palaeomagnetism in Vestfjella, Dronning Maud Land, East Antarctica. Geophysical Journal of the Royal Astronomical Society, 59(3), 529–537. https://doi.org/https://doi.org/10.1111/j.1365-246X.1979.tb02571.x

Thermal and alternating field demagnetization of oriented samples of Mesozoic lava flows (200–230 Myr) and dykes (154–172 Myr) collected from seven nunataks within the Vestfjella region, Dronning Maud Land, revealed stable directions of magnetization of normal and reverse polarity. Directional distributions of both polarities define tight groups along the same palaeomagnetic axis. Depending on whether the regional westward dip of the lava flows originated prior to, or after the intrusive igneous phase, two or one, respectively, palaeomagnetic pole(s) can be estimated. Both poles, however, are in general accord with previous Mesozoic poles from East Antarctica.

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Furnes, H. (1978). Basaltene i Vestfjella og Gondwanalands historie. Naturen, 102(6), 243–250.
Furnes, H., & Løvlie, R. (1978). An eruptional model for recent lava flow on Bouvetøya, South Atlantic Ocean. In Results from Norwegian Antarctic Research 1974-1977 (Vol. 169, pp. 103–108, ill. fig.). Norsk Polarinstitutt. https://brage.npolar.no/npolar-xmlui/handle/11250/173650

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Furnes, H., & Mitchell, J. G. (1978). Age relationships of Mesozoic basalt lava and dykes in Vestfjella, Dronning Maud Land, Antarctica. In Results from Norwegian Antarctic Research 1974-1977 (Vol. 169, pp. 45–68, ill. fig.). Norsk Polarinstitutt. https://brage.npolar.no/npolar-xmlui/handle/11250/173650

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Hjelle, A., Ohta, Y., & Winsnes, T. S. (1978). Stratigraphy and igneous petrology of Southern Heritage Range, Ellsworth Mountains, Antarctica. In Results from Norwegian Antarctic Research 1974-1977 (Vol. 169, pp. 5–43, ill. fig.). Norsk Polarinstitutt. https://brage.npolar.no/npolar-xmlui/handle/11250/173650

Sedimentary and magmatic rocks of Late Proterozoic to Late Paleozoic age, from the southern half of Ellsworth Mountains are described. Basic volcanic rocks, mainly agglomeratic, occur abundantly in the lower part of the succession, in the Minaret Group, and in the lower part of the Heritage Group, but are not recorded in the upper part of the Heritage Group. Due to this lithostratigraphic contrast a new classification is proposed: the Heritage Group including the Middle Horseshoe Formation and the Edson Hills Formation. A stratigraphic gap is evident above the Edson Hills Formation and a separate unit--the Dunbar Ridge Formation--is proposed. This formation is of Middle-Upper Cambrian age, with trilobite-bearing limestones. The structure is governed by a major anticline with a NW plunge in the north but almost horizontal in the south. Contrast of fold intensity and fold style below the youngest exposed unit, the Whiteout Conglomerate and a weathered surface above the Crashite Quartzite suggests a late Paleozoic deformation phase. Two phases of magmatism are distinguished. The pre-Middle Cambrian magmatism is dominantly K-alkalic and suggests the beginning of block subsidence at the early stage of a rift tectonics on a continental crust. The presumptive Late Paleozoic magmatism is N-alkalic and tholeiitic, and occurred after the main deformation; however the rocks were regionally metamorphosed in the actinolite-greenschist facies probably in late Paleozoic time. This magmatism is considered to represent an advanced stage of block tectonics. (Auth. mod.)

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Løvlie, R. (1978). Hva den fossile magnetiseringen i Vestfjella kan fortelle. Naturen, 102(6), 251–256.

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