The Re¤union Subchronozone at ODP Site 981 (Feni Drift, North Atlantic)
At Ocean Drilling Program Site 981, the Re¤union Subchron is recorded from the Marine Isotopic Stage (MIS) 81/ 82 boundary to MIS 79 as a single normal polarity zone spanning the 2.115^2.153-Ma interval. According to the age model, produced by matching the Site 981 N18O record to an orbitally-tuned...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.596.4123 2023-05-15T17:29:09+02:00 The Re¤union Subchronozone at ODP Site 981 (Feni Drift, North Atlantic) J. E. T. Channell A J. Labs A M. E. Raymo B The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.596.4123 http://web.clas.ufl.edu/users/jetc/publications/ChannelletalEPSL2003.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.596.4123 http://web.clas.ufl.edu/users/jetc/publications/ChannelletalEPSL2003.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://web.clas.ufl.edu/users/jetc/publications/ChannelletalEPSL2003.pdf 2003 Elsevier B.V. All rights reserved. Keywords magnetic stratigraphy isotope stratigraphy Re¤union Subchron North Atlantic Rockall Plateau Feni Drift text ftciteseerx 2016-01-08T13:45:15Z At Ocean Drilling Program Site 981, the Re¤union Subchron is recorded from the Marine Isotopic Stage (MIS) 81/ 82 boundary to MIS 79 as a single normal polarity zone spanning the 2.115^2.153-Ma interval. According to the age model, produced by matching the Site 981 N18O record to an orbitally-tuned reference record, the duration of the Re¤union Subchron (38 kyr) is almost four times that assumed in current geomagnetic polarity timescales. High interval sedimentation rates (18 cm/kyr) during MIS 81 at Site 981 have resulted in an unusually detailed record of the Subchron. Virtual geomagnetic poles during the onset and demise of the Re¤union Subchron trace a series of mainly anticlockwise loops over eastern Asia. Text North Atlantic Unknown Rockall Plateau ENVELOPE(-18.833,-18.833,56.333,56.333) |
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Open Polar |
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Unknown |
op_collection_id |
ftciteseerx |
language |
English |
topic |
2003 Elsevier B.V. All rights reserved. Keywords magnetic stratigraphy isotope stratigraphy Re¤union Subchron North Atlantic Rockall Plateau Feni Drift |
spellingShingle |
2003 Elsevier B.V. All rights reserved. Keywords magnetic stratigraphy isotope stratigraphy Re¤union Subchron North Atlantic Rockall Plateau Feni Drift J. E. T. Channell A J. Labs A M. E. Raymo B The Re¤union Subchronozone at ODP Site 981 (Feni Drift, North Atlantic) |
topic_facet |
2003 Elsevier B.V. All rights reserved. Keywords magnetic stratigraphy isotope stratigraphy Re¤union Subchron North Atlantic Rockall Plateau Feni Drift |
description |
At Ocean Drilling Program Site 981, the Re¤union Subchron is recorded from the Marine Isotopic Stage (MIS) 81/ 82 boundary to MIS 79 as a single normal polarity zone spanning the 2.115^2.153-Ma interval. According to the age model, produced by matching the Site 981 N18O record to an orbitally-tuned reference record, the duration of the Re¤union Subchron (38 kyr) is almost four times that assumed in current geomagnetic polarity timescales. High interval sedimentation rates (18 cm/kyr) during MIS 81 at Site 981 have resulted in an unusually detailed record of the Subchron. Virtual geomagnetic poles during the onset and demise of the Re¤union Subchron trace a series of mainly anticlockwise loops over eastern Asia. |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
J. E. T. Channell A J. Labs A M. E. Raymo B |
author_facet |
J. E. T. Channell A J. Labs A M. E. Raymo B |
author_sort |
J. E. T. Channell A |
title |
The Re¤union Subchronozone at ODP Site 981 (Feni Drift, North Atlantic) |
title_short |
The Re¤union Subchronozone at ODP Site 981 (Feni Drift, North Atlantic) |
title_full |
The Re¤union Subchronozone at ODP Site 981 (Feni Drift, North Atlantic) |
title_fullStr |
The Re¤union Subchronozone at ODP Site 981 (Feni Drift, North Atlantic) |
title_full_unstemmed |
The Re¤union Subchronozone at ODP Site 981 (Feni Drift, North Atlantic) |
title_sort |
re¤union subchronozone at odp site 981 (feni drift, north atlantic) |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.596.4123 http://web.clas.ufl.edu/users/jetc/publications/ChannelletalEPSL2003.pdf |
long_lat |
ENVELOPE(-18.833,-18.833,56.333,56.333) |
geographic |
Rockall Plateau |
geographic_facet |
Rockall Plateau |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_source |
http://web.clas.ufl.edu/users/jetc/publications/ChannelletalEPSL2003.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.596.4123 http://web.clas.ufl.edu/users/jetc/publications/ChannelletalEPSL2003.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766122779025866752 |