onr:"swepub:oai:lup.lub.lu.se:b287823e-bec3-41a6-ac6c-b956e0d15404"
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| Fältnamn | Indikatorer | Metadata |
|---|---|---|
| 000 | 03191naa a2200337 4500 | |
| 001 | oai:lup.lub.lu.se:b287823e-bec3-41a6-ac6c-b956e0d15404 | |
| 003 | SwePub | |
| 008 | 200805s1994 | |||||||||||000 ||eng| | |
| 024 | 7 | a https://lup.lub.lu.se/record/b287823e-bec3-41a6-ac6c-b956e0d154042 URI |
| 024 | 7 | a https://doi.org/10.1111/j.1502-3885.1994.tb00612.x2 DOI |
| 040 | a (SwePub)lu | |
| 041 | a engb eng | |
| 042 | 9 SwePub | |
| 072 | 7 | a art2 swepub-publicationtype |
| 072 | 7 | a ref2 swepub-contenttype |
| 100 | 1 | a Möller, Peru Lund University,Lunds universitet,Kvartärgeologi,Geologiska institutionen,Naturvetenskapliga fakulteten,Quaternary Sciences,Department of Geology,Faculty of Science4 aut0 (Swepub:lu)geol-pmo |
| 245 | 1 0 | a Late Quaternary glacial history of the west coast of Jameson Land, East Greenland |
| 264 | c 2008-01-16 | |
| 264 | 1 | b Wiley,c 1994 |
| 520 | a The Late Quaternary (c. 130000-10000 BP) glacial history of the central west coast of Jameson Land, East Greenland. is reconstructed through glacial stratigraphical studies. Seven major sedimentary units are described and defined. They represent two interglacial events (where one is the Holocene). one interstadial event and two glacial events. The older interglacial event comprises marine and fluvial sediments, and is correlated to the Langelandselv interglacial. corresponding to oxygen isotope sub-stage 5e. It is followed by an Early Weichselian major glaciation during the Aucellaelv stade. and subsequently by an Early Weichselian interstadial marine and deltaic event (the Hugin S0 interstade). Sediments relating to the Middle Weichselian have not been recognized in the area. The llugin S0 interstade deposits have been overrun by a Late Weichselian ice advance, during the Flakkerhuk stade. when the glacier. which probably was a thin, low gradient fjord glacier in Scoresby Sund, draped older sediments and landforms with a thin till. Subsequent to the final deglaciation, some time before 10 000 BP. the sea reached the marine limit around 70 m a , and early Holocene marine. fluvial and littoral sediments were deposited in the coastal areas. | |
| 650 | 7 | a NATURVETENSKAPx Geovetenskap och miljövetenskapx Geologi0 (SwePub)105042 hsv//swe |
| 650 | 7 | a NATURAL SCIENCESx Earth and Related Environmental Sciencesx Geology0 (SwePub)105042 hsv//eng |
| 700 | 1 | a Ingólfsson, Ólafuru University of Gothenburg,University of Iceland,University Centre in Svalbard4 aut |
| 700 | 1 | a Lyså, Astridu Geological Survey of Norway4 aut |
| 700 | 1 | a Funder, Su Natural History Museum of Denmark4 aut |
| 700 | 1 | a Björck, Svanteu Lund University,Lunds universitet,Kvartärgeologi,Geologiska institutionen,Naturvetenskapliga fakulteten,Quaternary Sciences,Department of Geology,Faculty of Science4 aut0 (Swepub:lu)geol-sbj |
| 710 | 2 | a Kvartärgeologib Geologiska institutionen4 org |
| 773 | 0 | t Boreasd : Wileyg 23, s. 447-458q 23<447-458x 1502-3885x 0300-9483 |
| 856 | 4 | u http://dx.doi.org/10.1111/j.1502-3885.1994.tb00612.xy FULLTEXT |
| 856 | 4 8 | u https://lup.lub.lu.se/record/b287823e-bec3-41a6-ac6c-b956e0d15404 |
| 856 | 4 8 | u https://doi.org/10.1111/j.1502-3885.1994.tb00612.x |
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