Sökning: WFRF:(Gool Jeroen A.M.) > (2007) > A multi-disciplinar...
Fältnamn | Indikatorer | Metadata |
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000 | 03154naa a2200493 4500 | |
001 | oai:DiVA.org:su-19299 | |
003 | SwePub | |
008 | 071101s2007 | |||||||||||000 ||eng| | |
024 | 7 | a https://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-192992 URI |
040 | a (SwePub)su | |
041 | a engb eng | |
042 | 9 SwePub | |
072 | 7 | a ref2 swepub-contenttype |
072 | 7 | a art2 swepub-publicationtype |
100 | 1 | a Bonow, Johan M.4 aut |
245 | 1 0 | a A multi-disciplinary study of Phanerozoic landscape development in West Greenland |
264 | 1 | c 2007 |
338 | a print2 rdacarrier | |
520 | a The western margin of the Greenland craton has been muchless stable in the Phanerozoic than previously thought. Thisnew insight has come from close integration of independentdata sets: geomorphological analysis of large-scale landscapes,apatite fission track analysis (AFTA), onshore and offshorestratigraphy and analysis of onshore fault and fracture sys -tems. Each data set records specific and unique parts of theevent chronology and is equally important to establish a con-sistent model. A key area for understanding the Mesozoic-Cenozoic landscape evolution and into the present is theuplifted part of the Nuussuaq Basin, where remnants of pla-nation surfaces cut across the Cretaceous to Eocene sedimen-tary and volcanic rocks. Our integrated analysis concludedthat the West Greenland mountains were formed by lateNeogene tectonic uplift (Fig. 1) and also provided newinsight into early Phanerozoic development. To understandour model, we present the different methods and the resultsthat can be deduced from them. | |
650 | 7 | a NATURVETENSKAPx Geovetenskap och miljövetenskapx Naturgeografi0 (SwePub)105072 hsv//swe |
650 | 7 | a NATURAL SCIENCESx Earth and Related Environmental Sciencesx Physical Geography0 (SwePub)105072 hsv//eng |
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 |
653 | a landscape development | |
653 | a palaeosurfaces | |
653 | a AFTA | |
653 | a faults and fractures | |
653 | a Physical geography | |
653 | a Naturgeografi | |
653 | a Historical geology and palaeontology | |
653 | a Historisk geologi och paleontologi | |
653 | a Solid earth geology and petrology | |
653 | a Berggrundsgeologi och petrologi | |
700 | 1 | a Japsen, Peter4 aut |
700 | 1 | a Green, Paul F.4 aut |
700 | 1 | a Wilson, Robert W.4 aut |
700 | 1 | a Chalmers, James A.4 aut |
700 | 1 | a Klint, Knud Erik S.4 aut |
700 | 1 | a Gool, Jeroen A.M.4 aut |
700 | 1 | a Lidmar-Bergström, Karnau Stockholms universitet,Institutionen för naturgeografi och kvartärgeologi (INK)4 aut0 (Swepub:su)karna |
700 | 1 | a Pedersen, Asger Ken4 aut |
710 | 2 | a Stockholms universitetb Institutionen för naturgeografi och kvartärgeologi (INK)4 org |
773 | 0 | t Geological Survey of Denmark and Greenland Bulletin: Review of Survey activities 2006g :13, s. 33-36q :13<33-36x 1604-8156 |
856 | 4 8 | u https://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-19299 |
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