Magnetostratigraphy of ODP sites 114-701 and 114-702 ...

During Leg 114 of the Ocean Drilling Program 12 holes were drilled at seven sites in the subantarctic South Atlantic Ocean. A major objective of this cruise was to document the development of the deep-water passageway that formed as the Meteor and Islas Orcadas rises rifted and spread apart. We repo...

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Main Authors: Clement, Bradford M, Hailwood, Ernie A
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 1991
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.734996
https://doi.pangaea.de/10.1594/PANGAEA.734996
id ftdatacite:10.1594/pangaea.734996
record_format openpolar
spelling ftdatacite:10.1594/pangaea.734996 2024-09-15T18:36:27+00:00 Magnetostratigraphy of ODP sites 114-701 and 114-702 ... Clement, Bradford M Hailwood, Ernie A 1991 application/zip https://dx.doi.org/10.1594/pangaea.734996 https://doi.pangaea.de/10.1594/PANGAEA.734996 en eng PANGAEA https://dx.doi.org/10.2973/odp.proc.sr.114.156.1991 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Drilling/drill rig Leg114 Joides Resolution Ocean Drilling Program ODP article Collection Supplementary Publication Series of Datasets 1991 ftdatacite https://doi.org/10.1594/pangaea.73499610.2973/odp.proc.sr.114.156.1991 2024-08-01T10:54:23Z During Leg 114 of the Ocean Drilling Program 12 holes were drilled at seven sites in the subantarctic South Atlantic Ocean. A major objective of this cruise was to document the development of the deep-water passageway that formed as the Meteor and Islas Orcadas rises rifted and spread apart. We report here the results of a magnetostratigraphic study of the sediments recovered at Site 701, a deep-water site located within the gateway, and Site 702, a shallow-water site located near the crest of the Islas Orcadas Rise. The sequence of Pliocene-Pleistocene reversals observed at Site 701 is readily correlated with the Brunhes Chron through Chron C3A. Although correlation is more difficult in the older sections at Site 701 because of coring gaps and the lack of tight biostratigraphic control, it is possible to correlate the late Miocene sequence of reversals with Chrons C4A and C5. The polarity sequence observed in the very weakly magnetized middle to upper Eocene nannofossil chalks recovered from Hole 702B is ... : Supplement to: Clement, Bradford M; Hailwood, Ernie A (1991): Magnetostratigraphy of sediments from sites 701 and 702. In: Ciesielski, PF; Kristoffersen, Y; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 114, 359-366 ... Article in Journal/Newspaper South Atlantic Ocean DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Drilling/drill rig
Leg114
Joides Resolution
Ocean Drilling Program ODP
spellingShingle Drilling/drill rig
Leg114
Joides Resolution
Ocean Drilling Program ODP
Clement, Bradford M
Hailwood, Ernie A
Magnetostratigraphy of ODP sites 114-701 and 114-702 ...
topic_facet Drilling/drill rig
Leg114
Joides Resolution
Ocean Drilling Program ODP
description During Leg 114 of the Ocean Drilling Program 12 holes were drilled at seven sites in the subantarctic South Atlantic Ocean. A major objective of this cruise was to document the development of the deep-water passageway that formed as the Meteor and Islas Orcadas rises rifted and spread apart. We report here the results of a magnetostratigraphic study of the sediments recovered at Site 701, a deep-water site located within the gateway, and Site 702, a shallow-water site located near the crest of the Islas Orcadas Rise. The sequence of Pliocene-Pleistocene reversals observed at Site 701 is readily correlated with the Brunhes Chron through Chron C3A. Although correlation is more difficult in the older sections at Site 701 because of coring gaps and the lack of tight biostratigraphic control, it is possible to correlate the late Miocene sequence of reversals with Chrons C4A and C5. The polarity sequence observed in the very weakly magnetized middle to upper Eocene nannofossil chalks recovered from Hole 702B is ... : Supplement to: Clement, Bradford M; Hailwood, Ernie A (1991): Magnetostratigraphy of sediments from sites 701 and 702. In: Ciesielski, PF; Kristoffersen, Y; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 114, 359-366 ...
format Article in Journal/Newspaper
author Clement, Bradford M
Hailwood, Ernie A
author_facet Clement, Bradford M
Hailwood, Ernie A
author_sort Clement, Bradford M
title Magnetostratigraphy of ODP sites 114-701 and 114-702 ...
title_short Magnetostratigraphy of ODP sites 114-701 and 114-702 ...
title_full Magnetostratigraphy of ODP sites 114-701 and 114-702 ...
title_fullStr Magnetostratigraphy of ODP sites 114-701 and 114-702 ...
title_full_unstemmed Magnetostratigraphy of ODP sites 114-701 and 114-702 ...
title_sort magnetostratigraphy of odp sites 114-701 and 114-702 ...
publisher PANGAEA
publishDate 1991
url https://dx.doi.org/10.1594/pangaea.734996
https://doi.pangaea.de/10.1594/PANGAEA.734996
genre South Atlantic Ocean
genre_facet South Atlantic Ocean
op_relation https://dx.doi.org/10.2973/odp.proc.sr.114.156.1991
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.73499610.2973/odp.proc.sr.114.156.1991
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