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Registros recuperados: 4
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MD 168 / AMOCINT IMAGES XVII on board R/V Marion Dufresne ArchiMer
Kissel, C; Kleiven, H; Morin, X; The Shipboard Scientific Party,.
Tipo: Text
Ano: 2008 URL: https://archimer.ifremer.fr/doc/00500/61158/64603.pdf
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Geomagnetic field behavior during the Iceland Basin and Laschamp geomagnetic excursions: A simple transitional field geometry? ArchiMer
Laj, C; Kissel, C; Roberts, Ap.
[1] We present four new records of the Iceland Basin Excursion (IBE) and five new records of the Laschamp Excursion (LE) obtained from rapidly deposited marine sediments in the North Atlantic Ocean, the Nordic Seas, the Gulf of Mexico, the South China Sea, and the southern Indian Ocean. Marked minima in relative paleointensity correspond with the paleomagnetic directional changes associated with all of the excursion records. The virtual geomagnetic pole (VGP) paths of the four IBE records are all similar. The VGPs move southward over Europe and Africa, reaching the southern hemisphere (three reach Antarctica), and then move to more eastern longitudes before returning northward over Australia and east Asia, describing a large counterclockwise loop. The same...
Tipo: Text Palavras-chave: Virtual geomagnetic paths.
Ano: 2006 URL: https://archimer.ifremer.fr/doc/00239/34977/33475.pdf
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Evolution of weathering patterns in the Indo-Burman Ranges over the last 280 kyr: Effects of sediment provenance on Sr-87/Sr-86 ratios tracer ArchiMer
Colin, C; Turpin, L; Blamart, D; Frank, N; Kissel, C; Duchamp, S.
A high-resolution study of mineralogy and major element geochemistry combined with Sr and Nd isotopes has been conducted on high sedimentation rate cores collected off the Irrawaddy River mouth in the Andaman Sea and the Bay of Bengal to reconstruct the erosional and weathering history of the Irrawaddy River basin. In both cores, epsilon Nd(0) values imply that both glacial and interglacial sediments share a common crustal source: the Irrawaddy River. Strong glacial/interglacial cycles are recorded by Sr-87/Sr-86: interglacial periods yield values between 0.713 and 0.717, whereas glacial periods show higher values between 0.717 and 0.719. Variations of the pedogenic clays (smectite and kaolinite) to primary mineral (feldspar, quartz, illite, and chlorite)...
Tipo: Text Palavras-chave: Sr and Nd isotopes; Major elements; Erosional history; Indo-Burman Ranges; Irrawaddy River.
Ano: 2006 URL: https://archimer.ifremer.fr/doc/00235/34579/33111.pdf
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Deep-water mass source and dynamic associated with rapid climatic variations during the last glacial stage in the North Atlantic: A multiproxy investigation of the detrital fraction of deep-sea sediments ArchiMer
Ballini, M; Kissel, C; Colin, C; Richter, T.
[1] In order to investigate North Atlantic Deep Water (NADW) dynamics and variability during the last glacial stage, a very high resolution multiproxy analysis of the detrital fraction of sediments deposited during Heinrich event 4 and Dansgaard-Oeschger cycles 8 and 7 has been conducted on three deep-sea cores. These cores are distributed along the path of the North Atlantic Deep Water from the Faeroe Shetland Channel to the Reykjanes ridge and the Irminger basin. The concentration in fine-grained magnetites, the Ti-content, and the smectite percentage within the clay minerals show similar and coeval fluctuations at each site and are comparable from one site to the other. This is the imprint of the detrital fraction originating from the northern basaltic...
Tipo: Text Palavras-chave: Glacial period; Dansgaard-Oeschger cycles; North Atlantic; Bottom water circulation; Magnetic properties; Clay minerals.
Ano: 2006 URL: https://archimer.ifremer.fr/doc/00235/34585/33077.pdf
Registros recuperados: 4
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