Paleomagnetic and rock magnetic characterization of ODP Leg 210 cores ...

We conducted an integrated paleomagnetic and rock magnetic study on cores recovered from Ocean Drilling Program Sites 1276 and 1277 of the Newfoundland Basin. Stable components of magnetization are determined from Cretaceous-aged sedimentary and basement cores after detailed thermal and alternating-...

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Main Authors: Zhao, Xixi, Galbrun, Bruno, Delius, Heike, Liu, Qingsong
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2007
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.776793
https://doi.pangaea.de/10.1594/PANGAEA.776793
id ftdatacite:10.1594/pangaea.776793
record_format openpolar
spelling ftdatacite:10.1594/pangaea.776793 2024-09-15T18:19:59+00:00 Paleomagnetic and rock magnetic characterization of ODP Leg 210 cores ... Zhao, Xixi Galbrun, Bruno Delius, Heike Liu, Qingsong 2007 application/zip https://dx.doi.org/10.1594/pangaea.776793 https://doi.pangaea.de/10.1594/PANGAEA.776793 en eng PANGAEA https://dx.doi.org/10.2973/odp.proc.sr.210.114.2007 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Composite Core Drilling/drill rig Leg210 Joides Resolution Ocean Drilling Program ODP Collection Supplementary Publication Series of Datasets article 2007 ftdatacite https://doi.org/10.1594/pangaea.77679310.2973/odp.proc.sr.210.114.2007 2024-09-02T08:42:43Z We conducted an integrated paleomagnetic and rock magnetic study on cores recovered from Ocean Drilling Program Sites 1276 and 1277 of the Newfoundland Basin. Stable components of magnetization are determined from Cretaceous-aged sedimentary and basement cores after detailed thermal and alternating-field demagnetization. Results from a series of rock magnetic measurements corroborate the demagnetization behavior and show that titanomagnetites are the main magnetic carrier. In view of the normal polarity of magnetization and radiometric dates for the sills at Site 1276 (~98 and ~105 Ma, both within the Cretaceous Normal Superchron) and for a gabbro intrusion in peridotite at Site 1277 (~126 Ma, Chron M1), our results suggest that the primary magnetization of the Cretaceous rocks is likely retained in these rocks. The overall magnetic inclination of lithologic Unit 2 in Hole 1277A between 143 and 180 meters below seafloor is 38°, implying significant (~35° counterclockwise, viewed to the north) rotation of the ... : Supplement to: Zhao, Xixi; Galbrun, Bruno; Delius, Heike; Liu, Qingsong (2007): Paleolatitude inferred from Cretaceous sedimentary and igneous cores recovered from Leg 210, Newfoundland margin. In: Tucholke, BE; Sibuet, J-C; Klaus, A (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 210, 1-37 ... Article in Journal/Newspaper Newfoundland DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Composite Core
Drilling/drill rig
Leg210
Joides Resolution
Ocean Drilling Program ODP
spellingShingle Composite Core
Drilling/drill rig
Leg210
Joides Resolution
Ocean Drilling Program ODP
Zhao, Xixi
Galbrun, Bruno
Delius, Heike
Liu, Qingsong
Paleomagnetic and rock magnetic characterization of ODP Leg 210 cores ...
topic_facet Composite Core
Drilling/drill rig
Leg210
Joides Resolution
Ocean Drilling Program ODP
description We conducted an integrated paleomagnetic and rock magnetic study on cores recovered from Ocean Drilling Program Sites 1276 and 1277 of the Newfoundland Basin. Stable components of magnetization are determined from Cretaceous-aged sedimentary and basement cores after detailed thermal and alternating-field demagnetization. Results from a series of rock magnetic measurements corroborate the demagnetization behavior and show that titanomagnetites are the main magnetic carrier. In view of the normal polarity of magnetization and radiometric dates for the sills at Site 1276 (~98 and ~105 Ma, both within the Cretaceous Normal Superchron) and for a gabbro intrusion in peridotite at Site 1277 (~126 Ma, Chron M1), our results suggest that the primary magnetization of the Cretaceous rocks is likely retained in these rocks. The overall magnetic inclination of lithologic Unit 2 in Hole 1277A between 143 and 180 meters below seafloor is 38°, implying significant (~35° counterclockwise, viewed to the north) rotation of the ... : Supplement to: Zhao, Xixi; Galbrun, Bruno; Delius, Heike; Liu, Qingsong (2007): Paleolatitude inferred from Cretaceous sedimentary and igneous cores recovered from Leg 210, Newfoundland margin. In: Tucholke, BE; Sibuet, J-C; Klaus, A (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 210, 1-37 ...
format Article in Journal/Newspaper
author Zhao, Xixi
Galbrun, Bruno
Delius, Heike
Liu, Qingsong
author_facet Zhao, Xixi
Galbrun, Bruno
Delius, Heike
Liu, Qingsong
author_sort Zhao, Xixi
title Paleomagnetic and rock magnetic characterization of ODP Leg 210 cores ...
title_short Paleomagnetic and rock magnetic characterization of ODP Leg 210 cores ...
title_full Paleomagnetic and rock magnetic characterization of ODP Leg 210 cores ...
title_fullStr Paleomagnetic and rock magnetic characterization of ODP Leg 210 cores ...
title_full_unstemmed Paleomagnetic and rock magnetic characterization of ODP Leg 210 cores ...
title_sort paleomagnetic and rock magnetic characterization of odp leg 210 cores ...
publisher PANGAEA
publishDate 2007
url https://dx.doi.org/10.1594/pangaea.776793
https://doi.pangaea.de/10.1594/PANGAEA.776793
genre Newfoundland
genre_facet Newfoundland
op_relation https://dx.doi.org/10.2973/odp.proc.sr.210.114.2007
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.77679310.2973/odp.proc.sr.210.114.2007
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