Grain size and description on gravity core samples from ANT-IV/2 expedition to the Bransfield Strait
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| Autori principali: | , |
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| Natura: | Dataset Open Access |
| Lingua: | en |
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PANGAEA
2010
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| _version_ | 1867170457806962688 |
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| author | van Enst, J W Laban, C |
| author_facet | van Enst, J W Laban, C |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | From the above and the grafical results it can be concluded that cores in the research area are locally dominated by turbiditic sequences, which can be observed by a strong increase in coarser sediment (>35 µm). These coarser intercalations are lacking in the vicinity of basaltic seamounts, probably due to a shadowing effect of the seamounts. The infill of the King George Basin might be dominated by a north eastern current. Sedimentary structures as observed in the cores are often lacking or vague due to hydrothermal effects (Suess, L, 1986). |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_738447 |
| institution | PANGAEA |
| language | en |
| publishDate | 2010 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Grain size and description on gravity core samples from ANT-IV/2 expedition to the Bransfield Strait van Enst, J W Laban, C ANT-IV/2; AWI_Paleo; Bransfield Strait; Gravity corer (Kiel type); King George Island, Antarctic Peninsula; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; PS08; PS08/279; PS08/284; PS08/291; PS08/295; PS08/306; PS1327-1; PS1333-1; PS1340-1; PS1341-1; PS1342-1; PS1343-1; PS1346-1; PS1347-1; PS1357-2; SL From the above and the grafical results it can be concluded that cores in the research area are locally dominated by turbiditic sequences, which can be observed by a strong increase in coarser sediment (>35 µm). These coarser intercalations are lacking in the vicinity of basaltic seamounts, probably due to a shadowing effect of the seamounts. The infill of the King George Basin might be dominated by a north eastern current. Sedimentary structures as observed in the cores are often lacking or vague due to hydrothermal effects (Suess, L, 1986). |
| title | Grain size and description on gravity core samples from ANT-IV/2 expedition to the Bransfield Strait |
| topic | ANT-IV/2; AWI_Paleo; Bransfield Strait; Gravity corer (Kiel type); King George Island, Antarctic Peninsula; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; PS08; PS08/279; PS08/284; PS08/291; PS08/295; PS08/306; PS1327-1; PS1333-1; PS1340-1; PS1341-1; PS1342-1; PS1343-1; PS1346-1; PS1347-1; PS1357-2; SL |
| url | https://doi.org/10.1594/PANGAEA.738447 |