Magnetic susceptibility and documentation of sediment cores from the Antarctic Peninsula Pacific margin ...
The effects of glaciation on sediment drifts is recognised from marked sedimentary facies variation in deep sea cores taken from the continental rise of the Antarctic Peninsula Pacific margin. Nineteen sediment cores were visually described, logged for magnetic susceptibility, and X-radiographed. Ab...
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ftdatacite:10.1594/pangaea.671563 2024-09-15T17:47:09+00:00 Magnetic susceptibility and documentation of sediment cores from the Antarctic Peninsula Pacific margin ... Lucchi, Renata G Rebesco, Michele Camerlenghi, Angelo Busetti, Martina Tomadin, Luciano Villa, Giuliana Persico, Davide Morigi, Caterina Bonci, M C Giorgetti, Giovanna 2007 application/zip https://dx.doi.org/10.1594/pangaea.671563 https://doi.pangaea.de/10.1594/PANGAEA.671563 en eng PANGAEA https://dx.doi.org/10.1016/s0025-3227(02)00470-x Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Gravity corer SEDANO-II Explorer article Collection Supplementary Publication Series of Datasets 2007 ftdatacite https://doi.org/10.1594/pangaea.67156310.1016/s0025-3227(02)00470-x 2024-08-01T10:59:11Z The effects of glaciation on sediment drifts is recognised from marked sedimentary facies variation in deep sea cores taken from the continental rise of the Antarctic Peninsula Pacific margin. Nineteen sediment cores were visually described, logged for magnetic susceptibility, and X-radiographed. About 1000 analyses were performed for grain size, clay minerals and biostratigraphy (foraminifera, nannofossils and diatoms). Four sediment types associated with distinct sedimentary processes are recognised based on textural/compositional analysis. (1) Hemipelagic mud forms the bulk of the interglacial sediment, and accumulated from the pelagic settling of bioclasts and ice-rafted/windtransported detritus. (2) Terrigenous mud forms the bulk of the glacial sediment, and accumulated from a combination of sedimentary processes including turbidity currents, turbid plumes, and bottom current reworking of nepheloid layers. (3) Silty deposits occurring as laminated layers and lenses, represent the lateral spillout of ... : Supplement to: Lucchi, Renata G; Rebesco, Michele; Camerlenghi, Angelo; Busetti, Martina; Tomadin, Luciano; Villa, Giuliana; Persico, Davide; Morigi, Caterina; Bonci, M C; Giorgetti, Giovanna (2002): Mid-late Pleistocene glacimarine sedimentary processes of a high-latitude, deep-sea sediment drift (Antarctic Peninsula Pacific margin). Marine Geology, 189(3-4), 343-370 ... Article in Journal/Newspaper Antarc* Antarctic Antarctic Peninsula DataCite |
institution |
Open Polar |
collection |
DataCite |
op_collection_id |
ftdatacite |
language |
English |
topic |
Gravity corer SEDANO-II Explorer |
spellingShingle |
Gravity corer SEDANO-II Explorer Lucchi, Renata G Rebesco, Michele Camerlenghi, Angelo Busetti, Martina Tomadin, Luciano Villa, Giuliana Persico, Davide Morigi, Caterina Bonci, M C Giorgetti, Giovanna Magnetic susceptibility and documentation of sediment cores from the Antarctic Peninsula Pacific margin ... |
topic_facet |
Gravity corer SEDANO-II Explorer |
description |
The effects of glaciation on sediment drifts is recognised from marked sedimentary facies variation in deep sea cores taken from the continental rise of the Antarctic Peninsula Pacific margin. Nineteen sediment cores were visually described, logged for magnetic susceptibility, and X-radiographed. About 1000 analyses were performed for grain size, clay minerals and biostratigraphy (foraminifera, nannofossils and diatoms). Four sediment types associated with distinct sedimentary processes are recognised based on textural/compositional analysis. (1) Hemipelagic mud forms the bulk of the interglacial sediment, and accumulated from the pelagic settling of bioclasts and ice-rafted/windtransported detritus. (2) Terrigenous mud forms the bulk of the glacial sediment, and accumulated from a combination of sedimentary processes including turbidity currents, turbid plumes, and bottom current reworking of nepheloid layers. (3) Silty deposits occurring as laminated layers and lenses, represent the lateral spillout of ... : Supplement to: Lucchi, Renata G; Rebesco, Michele; Camerlenghi, Angelo; Busetti, Martina; Tomadin, Luciano; Villa, Giuliana; Persico, Davide; Morigi, Caterina; Bonci, M C; Giorgetti, Giovanna (2002): Mid-late Pleistocene glacimarine sedimentary processes of a high-latitude, deep-sea sediment drift (Antarctic Peninsula Pacific margin). Marine Geology, 189(3-4), 343-370 ... |
format |
Article in Journal/Newspaper |
author |
Lucchi, Renata G Rebesco, Michele Camerlenghi, Angelo Busetti, Martina Tomadin, Luciano Villa, Giuliana Persico, Davide Morigi, Caterina Bonci, M C Giorgetti, Giovanna |
author_facet |
Lucchi, Renata G Rebesco, Michele Camerlenghi, Angelo Busetti, Martina Tomadin, Luciano Villa, Giuliana Persico, Davide Morigi, Caterina Bonci, M C Giorgetti, Giovanna |
author_sort |
Lucchi, Renata G |
title |
Magnetic susceptibility and documentation of sediment cores from the Antarctic Peninsula Pacific margin ... |
title_short |
Magnetic susceptibility and documentation of sediment cores from the Antarctic Peninsula Pacific margin ... |
title_full |
Magnetic susceptibility and documentation of sediment cores from the Antarctic Peninsula Pacific margin ... |
title_fullStr |
Magnetic susceptibility and documentation of sediment cores from the Antarctic Peninsula Pacific margin ... |
title_full_unstemmed |
Magnetic susceptibility and documentation of sediment cores from the Antarctic Peninsula Pacific margin ... |
title_sort |
magnetic susceptibility and documentation of sediment cores from the antarctic peninsula pacific margin ... |
publisher |
PANGAEA |
publishDate |
2007 |
url |
https://dx.doi.org/10.1594/pangaea.671563 https://doi.pangaea.de/10.1594/PANGAEA.671563 |
genre |
Antarc* Antarctic Antarctic Peninsula |
genre_facet |
Antarc* Antarctic Antarctic Peninsula |
op_relation |
https://dx.doi.org/10.1016/s0025-3227(02)00470-x |
op_rights |
Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
op_doi |
https://doi.org/10.1594/pangaea.67156310.1016/s0025-3227(02)00470-x |
_version_ |
1810495882954539008 |