Distribution of clay minerals in ODP Hole 120-751A (Table 1) ...
The purpose of this paper is to present data from a clay mineralogy investigation of the sediments analyzed for ice-rafted debris (IRD) from Hole 751A (see Breza, 1992, doi:10.2973/odp.proc.sr.120.136.1992). This data is significant in that the change in clay mineralogy may provide information about...
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ftdatacite:10.1594/pangaea.758929 2024-09-15T17:46:59+00:00 Distribution of clay minerals in ODP Hole 120-751A (Table 1) ... Breza, James R 1992 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.758929 https://doi.pangaea.de/10.1594/PANGAEA.758929 en eng PANGAEA https://dx.doi.org/10.2973/odp.proc.sr.120.135.1992 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Sample code/label DEPTH, sediment/rock Smectite Illite Chlorite+Kaolinite Silica, amorphous Drilling/drill rig DSDP/ODP/IODP sample designation X-ray diffraction XRD Leg120 Joides Resolution Ocean Drilling Program ODP dataset Supplementary Dataset Dataset 1992 ftdatacite https://doi.org/10.1594/pangaea.75892910.2973/odp.proc.sr.120.135.1992 2024-08-01T10:59:28Z The purpose of this paper is to present data from a clay mineralogy investigation of the sediments analyzed for ice-rafted debris (IRD) from Hole 751A (see Breza, 1992, doi:10.2973/odp.proc.sr.120.136.1992). This data is significant in that the change in clay mineralogy may provide information about the Neogene evolution of climate and oceanic circulation near the Kerguelen Plateau and adjacent to Prydz Bay, Antarctica. Site 751 is located in the central part of the Raggatt Basin on the Southern Kerguelen Plateau in 1633.8 m of water (57°43.56'S, 79°48.89'E). The plateau is a structural high isolated from any continental input by means of turbidities or nepheloid transport. It is bounded to the northeast by the Australian-Antarctic Basin, to the southwest by the African-Antarctic Basin, and to the northwest by the Crozet Basin. To the south it is separated from Antarctica by the Princess Elizabeth Trough.Site 751 consists of two lithologic units. Unit I is composed of 40 m of upper Pleistocene to lower ... : X = present, - = not present ... Dataset Antarc* Antarctic Antarctica Prydz Bay DataCite |
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Open Polar |
collection |
DataCite |
op_collection_id |
ftdatacite |
language |
English |
topic |
Sample code/label DEPTH, sediment/rock Smectite Illite Chlorite+Kaolinite Silica, amorphous Drilling/drill rig DSDP/ODP/IODP sample designation X-ray diffraction XRD Leg120 Joides Resolution Ocean Drilling Program ODP |
spellingShingle |
Sample code/label DEPTH, sediment/rock Smectite Illite Chlorite+Kaolinite Silica, amorphous Drilling/drill rig DSDP/ODP/IODP sample designation X-ray diffraction XRD Leg120 Joides Resolution Ocean Drilling Program ODP Breza, James R Distribution of clay minerals in ODP Hole 120-751A (Table 1) ... |
topic_facet |
Sample code/label DEPTH, sediment/rock Smectite Illite Chlorite+Kaolinite Silica, amorphous Drilling/drill rig DSDP/ODP/IODP sample designation X-ray diffraction XRD Leg120 Joides Resolution Ocean Drilling Program ODP |
description |
The purpose of this paper is to present data from a clay mineralogy investigation of the sediments analyzed for ice-rafted debris (IRD) from Hole 751A (see Breza, 1992, doi:10.2973/odp.proc.sr.120.136.1992). This data is significant in that the change in clay mineralogy may provide information about the Neogene evolution of climate and oceanic circulation near the Kerguelen Plateau and adjacent to Prydz Bay, Antarctica. Site 751 is located in the central part of the Raggatt Basin on the Southern Kerguelen Plateau in 1633.8 m of water (57°43.56'S, 79°48.89'E). The plateau is a structural high isolated from any continental input by means of turbidities or nepheloid transport. It is bounded to the northeast by the Australian-Antarctic Basin, to the southwest by the African-Antarctic Basin, and to the northwest by the Crozet Basin. To the south it is separated from Antarctica by the Princess Elizabeth Trough.Site 751 consists of two lithologic units. Unit I is composed of 40 m of upper Pleistocene to lower ... : X = present, - = not present ... |
format |
Dataset |
author |
Breza, James R |
author_facet |
Breza, James R |
author_sort |
Breza, James R |
title |
Distribution of clay minerals in ODP Hole 120-751A (Table 1) ... |
title_short |
Distribution of clay minerals in ODP Hole 120-751A (Table 1) ... |
title_full |
Distribution of clay minerals in ODP Hole 120-751A (Table 1) ... |
title_fullStr |
Distribution of clay minerals in ODP Hole 120-751A (Table 1) ... |
title_full_unstemmed |
Distribution of clay minerals in ODP Hole 120-751A (Table 1) ... |
title_sort |
distribution of clay minerals in odp hole 120-751a (table 1) ... |
publisher |
PANGAEA |
publishDate |
1992 |
url |
https://dx.doi.org/10.1594/pangaea.758929 https://doi.pangaea.de/10.1594/PANGAEA.758929 |
genre |
Antarc* Antarctic Antarctica Prydz Bay |
genre_facet |
Antarc* Antarctic Antarctica Prydz Bay |
op_relation |
https://dx.doi.org/10.2973/odp.proc.sr.120.135.1992 |
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.75892910.2973/odp.proc.sr.120.135.1992 |
_version_ |
1810495446504701952 |