Magnetostratigraphy of DSDP Leg 94 sediments ...
The primary objective of DSDP Leg 94 was to obtain continuous paleoclimatic records along a roughly north-south transect in the North Atlantic. The magnetostratigraphy of 21 holes at 6 sites cored with the hydraulic piston corer and extended-core-barrel corer is presented here and establishes an ind...
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Online Access: | https://dx.doi.org/10.1594/pangaea.788554 https://doi.pangaea.de/10.1594/PANGAEA.788554 |
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ftdatacite:10.1594/pangaea.788554 2024-09-15T18:23:39+00:00 Magnetostratigraphy of DSDP Leg 94 sediments ... Clement, Bradford M Robinson, Frank 1987 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.788554 https://doi.pangaea.de/10.1594/PANGAEA.788554 en eng PANGAEA https://dx.doi.org/10.2973/dsdp.proc.94.112.1987 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Event label Elevation of event Latitude of event Longitude of event Sample code/label Sample code/label 2 Ageprofile Datum Description Depth, top/min Depth, bottom/max DEPTH, sediment/rock Age model Drilling/drill rig DSDP/ODP/IODP sample designation Leg94 Glomar Challenger Deep Sea Drilling Project DSDP dataset Supplementary Dataset Dataset 1987 ftdatacite https://doi.org/10.1594/pangaea.78855410.2973/dsdp.proc.94.112.1987 2024-08-01T10:57:37Z The primary objective of DSDP Leg 94 was to obtain continuous paleoclimatic records along a roughly north-south transect in the North Atlantic. The magnetostratigraphy of 21 holes at 6 sites cored with the hydraulic piston corer and extended-core-barrel corer is presented here and establishes an independent chronology for these sediments. Nearly complete records were obtained for the last 2.5 m.y.; in addition, deeper drilling at three sites to satisfy tectonic and paleoceanographic objectives produced older sections suitable for magnetostratigraphic study, allowing first-order correlations of the polarity sequences with calcareous and siliceous micro fossil events.The sections with high sediment accumulation rates yielded very detailed records of polarity history and allowed three short normal-polarity zones within the Matuyama Chronozone to be detected, in addition to the Jaramillo and Olduvai subchronozones. A short reversed-polarity zone also occurs, within the upper intervals of the Gauss Chronozone. ... : Supplement to: Clement, Bradford M; Robinson, Frank (1987): The magnetostratigraphy of Leg 94 sediments. In: Ruddiman, WF; Kidd, RB; Thomas, E; et al. (eds.), Initial Reports of the Deep Sea Drilling Project, Washington (U.S. Govt. Printing Office), 94, 635-650 ... Dataset North Atlantic DataCite |
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Open Polar |
collection |
DataCite |
op_collection_id |
ftdatacite |
language |
English |
topic |
Event label Elevation of event Latitude of event Longitude of event Sample code/label Sample code/label 2 Ageprofile Datum Description Depth, top/min Depth, bottom/max DEPTH, sediment/rock Age model Drilling/drill rig DSDP/ODP/IODP sample designation Leg94 Glomar Challenger Deep Sea Drilling Project DSDP |
spellingShingle |
Event label Elevation of event Latitude of event Longitude of event Sample code/label Sample code/label 2 Ageprofile Datum Description Depth, top/min Depth, bottom/max DEPTH, sediment/rock Age model Drilling/drill rig DSDP/ODP/IODP sample designation Leg94 Glomar Challenger Deep Sea Drilling Project DSDP Clement, Bradford M Robinson, Frank Magnetostratigraphy of DSDP Leg 94 sediments ... |
topic_facet |
Event label Elevation of event Latitude of event Longitude of event Sample code/label Sample code/label 2 Ageprofile Datum Description Depth, top/min Depth, bottom/max DEPTH, sediment/rock Age model Drilling/drill rig DSDP/ODP/IODP sample designation Leg94 Glomar Challenger Deep Sea Drilling Project DSDP |
description |
The primary objective of DSDP Leg 94 was to obtain continuous paleoclimatic records along a roughly north-south transect in the North Atlantic. The magnetostratigraphy of 21 holes at 6 sites cored with the hydraulic piston corer and extended-core-barrel corer is presented here and establishes an independent chronology for these sediments. Nearly complete records were obtained for the last 2.5 m.y.; in addition, deeper drilling at three sites to satisfy tectonic and paleoceanographic objectives produced older sections suitable for magnetostratigraphic study, allowing first-order correlations of the polarity sequences with calcareous and siliceous micro fossil events.The sections with high sediment accumulation rates yielded very detailed records of polarity history and allowed three short normal-polarity zones within the Matuyama Chronozone to be detected, in addition to the Jaramillo and Olduvai subchronozones. A short reversed-polarity zone also occurs, within the upper intervals of the Gauss Chronozone. ... : Supplement to: Clement, Bradford M; Robinson, Frank (1987): The magnetostratigraphy of Leg 94 sediments. In: Ruddiman, WF; Kidd, RB; Thomas, E; et al. (eds.), Initial Reports of the Deep Sea Drilling Project, Washington (U.S. Govt. Printing Office), 94, 635-650 ... |
format |
Dataset |
author |
Clement, Bradford M Robinson, Frank |
author_facet |
Clement, Bradford M Robinson, Frank |
author_sort |
Clement, Bradford M |
title |
Magnetostratigraphy of DSDP Leg 94 sediments ... |
title_short |
Magnetostratigraphy of DSDP Leg 94 sediments ... |
title_full |
Magnetostratigraphy of DSDP Leg 94 sediments ... |
title_fullStr |
Magnetostratigraphy of DSDP Leg 94 sediments ... |
title_full_unstemmed |
Magnetostratigraphy of DSDP Leg 94 sediments ... |
title_sort |
magnetostratigraphy of dsdp leg 94 sediments ... |
publisher |
PANGAEA |
publishDate |
1987 |
url |
https://dx.doi.org/10.1594/pangaea.788554 https://doi.pangaea.de/10.1594/PANGAEA.788554 |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_relation |
https://dx.doi.org/10.2973/dsdp.proc.94.112.1987 |
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.78855410.2973/dsdp.proc.94.112.1987 |
_version_ |
1810463899381661696 |