Heavy mineral investigations from surface sediments of the East Greenland continental margin
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| Format: | Dataset Open Access |
| Langue: | en |
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PANGAEA
2008
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| _version_ | 1867167660190466048 |
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| author | Grafenauer, Ingo Stein, Ruediger Fütterer, Dieter K |
| author_facet | Grafenauer, Ingo Stein, Ruediger Fütterer, Dieter K |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | During the expeditions ARK-VII/1, ARK-VII/3 and ARK-Xl2 sediment cores were taken by "RV Polarstern" from the shelf and the fjords of East Greenland and the Greenland Sea. The magnetic susceptibility and heavy mineral were determined at 48 surface sediment samples from undisturbed box cores. The main objective of this study was the identification of source areas and transport processes of terrigenous sediments at the East Greenland continental margin. The results can be summarized as lollows: 1a) Magnetic susceptibility in the North Atlantic is useful to detect delivery regions of the material transported by currents. b) The magnetic susceptibility is controlled by the ferromagnetic particles of the silt fraction. c) There are four important source areas: . The ferromagnetic particles of the box core PS2644-2 are transported from the Iceland Archipelago. . The material from the Geiki-Plateau effects the magnetic susceptibility in the Scoresby Sund Basin. . The magnetic susceptibility in the shelf regions in the North are produced by material from the fjords. . The ferromagnetic particles in the Greenland Sea are derived from the Mid Atlantic Ridges in the east. d) It is possible to determine the rock type, which delivers the ferromagnetic material because of differences in magnetic susceptibility of different intensity. . The erosion of the basalts of the Geiki-Plateau and the basalts of the Mid Atlantic ridges produce the high magnetic susceptibility in the south. . The magnetic susceptibility on the shelf in the north are probably produced by erosionproducts of the gneises of East Greenland. (2a) Heavy mineral assemblages show a significant difference between material transported by the Transpolar Drift from the Eurasian shelf regions (amphiboles, clinopyroxene, orthopyroxene) and material derived from East Greenland (garnets and opaque minerals). Transport via ice is dominant. b) lt is also possible to show different petrographic provenances (volcanic and metamorphic provenances). These associations verify the source areas. c) The information of heavy mineral composition gives no more detailed hint on the rock type or rock formation in the source area, due to mixing processes, large area of investigation and the sample quantity. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_701354 |
| institution | PANGAEA |
| language | en |
| publishDate | 2008 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Heavy mineral investigations from surface sediments of the East Greenland continental margin Grafenauer, Ingo Stein, Ruediger Fütterer, Dieter K ARK-VII/1; ARK-VII/3b; ARK-X/2; AWI_Paleo; Denmark Strait; Dickson Fjord, East Greenland; East Greenland Sea; Giant box corer; GIK21845-2 PS17/010; GIK21845-3 PS17/010; GIK21852-1 PS17/018; GIK21857-1 PS17/024; GIK21864-1 PS17/035; GIK21873-1 PS17/044; GIK21875-7 PS17/047; GIK21876-1 PS17/048; GIK21877-1 PS17/049; GIK21882-1 PS17/056; GIK21892-1 PS17/067; GIK21893-1 PS17/068; GIK21894-7 PS17/069; GIK21895-9 PS17/070a; GIK21898-6 PS17/073; GIK21900-7 PS17/075; GIK21901-1 PS17/076; GIK21903-1 PS17/078; GKG; Gravity corer (Kiel type); Greenland Sea; Greenland Shelf; Greenland Slope; Hochstetter Bugten, East Greenland; Kaiser-Franz-Josef-Fjord, East Greenland; KAL; Kasten corer; Kolbeinsey Ridge; Kong-Oskar-Fjord, East Greenland; Norwegian-Greenland Sea; Norwegian Sea; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; PS17; PS17/241; PS17/245; PS17/247; PS17/248; PS17/250; PS17/251; PS17/252; PS17/260; PS17/266; PS17/274; PS17/281; PS17/285; PS17/286; PS17/289; PS1845-2; PS1845-3; PS1852-1; PS1857-1; PS1864-1; PS1873-1; PS1875-7; PS1876-1; PS1877-1; PS1882-1; PS1892-1; PS1893-1; PS1894-7; PS1895-9; PS1898-6; PS1900-7; PS1901-1; PS1903-1; PS1918-2; PS1922-2; PS1923-1; PS1924-2; PS1926-2; PS1927-1; PS1928-1; PS1931-1; PS1935-1; PS1939-1; PS1943-1; PS1946-1; PS1947-1; PS1947-2; PS1950-1; PS2613-1; PS2616-7; PS2619-6; PS2621-3; PS2622-4; PS2625-1; PS2629-2; PS2631-2; PS2632-7; PS2634-5; PS2638-6; PS2639-2; PS2641-5; PS2643-5; PS2644-2; PS2645-5; PS31; PS31/113; PS31/116; PS31/122; PS31/127; PS31/128; PS31/131; PS31/137; PS31/140; PS31/141; PS31/143; PS31/150; PS31/151; PS31/154; PS31/156; PS31/160; PS31/161; Scoresby Sund; SL; Vesteris Banken During the expeditions ARK-VII/1, ARK-VII/3 and ARK-Xl2 sediment cores were taken by "RV Polarstern" from the shelf and the fjords of East Greenland and the Greenland Sea. The magnetic susceptibility and heavy mineral were determined at 48 surface sediment samples from undisturbed box cores. The main objective of this study was the identification of source areas and transport processes of terrigenous sediments at the East Greenland continental margin. The results can be summarized as lollows: 1a) Magnetic susceptibility in the North Atlantic is useful to detect delivery regions of the material transported by currents. b) The magnetic susceptibility is controlled by the ferromagnetic particles of the silt fraction. c) There are four important source areas: . The ferromagnetic particles of the box core PS2644-2 are transported from the Iceland Archipelago. . The material from the Geiki-Plateau effects the magnetic susceptibility in the Scoresby Sund Basin. . The magnetic susceptibility in the shelf regions in the North are produced by material from the fjords. . The ferromagnetic particles in the Greenland Sea are derived from the Mid Atlantic Ridges in the east. d) It is possible to determine the rock type, which delivers the ferromagnetic material because of differences in magnetic susceptibility of different intensity. . The erosion of the basalts of the Geiki-Plateau and the basalts of the Mid Atlantic ridges produce the high magnetic susceptibility in the south. . The magnetic susceptibility on the shelf in the north are probably produced by erosionproducts of the gneises of East Greenland. (2a) Heavy mineral assemblages show a significant difference between material transported by the Transpolar Drift from the Eurasian shelf regions (amphiboles, clinopyroxene, orthopyroxene) and material derived from East Greenland (garnets and opaque minerals). Transport via ice is dominant. b) lt is also possible to show different petrographic provenances (volcanic and metamorphic provenances). These associations verify the source areas. c) The information of heavy mineral composition gives no more detailed hint on the rock type or rock formation in the source area, due to mixing processes, large area of investigation and the sample quantity. |
| title | Heavy mineral investigations from surface sediments of the East Greenland continental margin |
| topic | ARK-VII/1; ARK-VII/3b; ARK-X/2; AWI_Paleo; Denmark Strait; Dickson Fjord, East Greenland; East Greenland Sea; Giant box corer; GIK21845-2 PS17/010; GIK21845-3 PS17/010; GIK21852-1 PS17/018; GIK21857-1 PS17/024; GIK21864-1 PS17/035; GIK21873-1 PS17/044; GIK21875-7 PS17/047; GIK21876-1 PS17/048; GIK21877-1 PS17/049; GIK21882-1 PS17/056; GIK21892-1 PS17/067; GIK21893-1 PS17/068; GIK21894-7 PS17/069; GIK21895-9 PS17/070a; GIK21898-6 PS17/073; GIK21900-7 PS17/075; GIK21901-1 PS17/076; GIK21903-1 PS17/078; GKG; Gravity corer (Kiel type); Greenland Sea; Greenland Shelf; Greenland Slope; Hochstetter Bugten, East Greenland; Kaiser-Franz-Josef-Fjord, East Greenland; KAL; Kasten corer; Kolbeinsey Ridge; Kong-Oskar-Fjord, East Greenland; Norwegian-Greenland Sea; Norwegian Sea; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; PS17; PS17/241; PS17/245; PS17/247; PS17/248; PS17/250; PS17/251; PS17/252; PS17/260; PS17/266; PS17/274; PS17/281; PS17/285; PS17/286; PS17/289; PS1845-2; PS1845-3; PS1852-1; PS1857-1; PS1864-1; PS1873-1; PS1875-7; PS1876-1; PS1877-1; PS1882-1; PS1892-1; PS1893-1; PS1894-7; PS1895-9; PS1898-6; PS1900-7; PS1901-1; PS1903-1; PS1918-2; PS1922-2; PS1923-1; PS1924-2; PS1926-2; PS1927-1; PS1928-1; PS1931-1; PS1935-1; PS1939-1; PS1943-1; PS1946-1; PS1947-1; PS1947-2; PS1950-1; PS2613-1; PS2616-7; PS2619-6; PS2621-3; PS2622-4; PS2625-1; PS2629-2; PS2631-2; PS2632-7; PS2634-5; PS2638-6; PS2639-2; PS2641-5; PS2643-5; PS2644-2; PS2645-5; PS31; PS31/113; PS31/116; PS31/122; PS31/127; PS31/128; PS31/131; PS31/137; PS31/140; PS31/141; PS31/143; PS31/150; PS31/151; PS31/154; PS31/156; PS31/160; PS31/161; Scoresby Sund; SL; Vesteris Banken |
| url | https://doi.org/10.1594/PANGAEA.701354 |