Supplementary paleomagnetic data to: “Paleomagnetism in the Pannonian; Problems, Pitfalls, and Progress in using iron sulphides for magnetostratigraphy”
Cite as:
Kelder, Nick A.; Sant, Karin; van Dijk, Gijs A.; Lathouwers, Ymke Z.; Dekkers, Mark J.; Krijgsman, Wout; Magyar, Imre; Sztanó, Orsolya (2018): Supplementary paleomagnetic data to: “Paleomagnetism in the Pannonian; Problems, Pitfalls, and Progress in using iron sulphides for magnetostratigraphy”. GFZ Data Services. https://doi.org/10.5880/fidgeo.2018.007
Status
I N R E V I E W : Kelder, Nick A.; Sant, Karin; van Dijk, Gijs A.; Lathouwers, Ymke Z.; Dekkers, Mark J.; Krijgsman, Wout; Magyar, Imre; Sztanó, Orsolya (2018): Supplementary paleomagnetic data to: “Paleomagnetism in the Pannonian; Problems, Pitfalls, and Progress in using iron sulphides for magnetostratigraphy”. GFZ Data Services. https://doi.org/10.5880/fidgeo.2018.007
Abstract
This dataset contains the paleomagnetic supplementary material to the article Kelder et al. (subm.), which presents a magnetostratigraphic correlation of Late Miocene lacustrine sediments based on multi-polarity greigite. The multi-polarity is visible in most thermal paleomagnetic results (Zijderveld diagrams) by antipodal high and medium temperature components, while only one magnetic component was visible in the alternating field demagnetization diagrams. Based on this complex behavior, a tailored demagnetization approach was developed to allow for reliable magnetostratigraphic dating of lacustrine sediments.
The dataset includes demagnetization data from four drill cores located nearby Paks, Hungary. They were not oriented, meaning that only the inclination could be used for paleomagnetism. The measurements took place at the Paleomagnetic Laboratory Fort Hoofddijk in Utrecht University, The Netherlands. For details about the methodology the reader is referred to the methodology in Kelder et al. (subm).
Three types of data are distinguished:
• Thermal demagnetization results (.th files)
• Alternating field demagnetization results (.af files).
• Interpreted magnetic vectors for demagnetization files (.dir files)
The .th, .af. and .dir files can be viewed with Notepad or similar programs, and analyzed via the Open Source platform Paleomagnetism.org (Koymans et al., 2016). The .dir files only exist for the cores PAET-30 and PAET-34, because these were interpreted in detail, while the material of the other cores (PAET-26, 27) were mainly used for rock magnetic purposes.
Finally, an overview of the data files, abbreviations and sample codes is provided in the data description file.
Authors
Kelder, Nick A.;Utrecht University, The Netherlands
title: Supplementary paleomagnetic data to: “Paleomagnetism in the Pannonian; Problems, Pitfalls, and Progress in using iron sulphides for magnetostratigraphy”
publisher: GFZ Data Services
publicationYear: 2018
subjects
subject: magnetostratigraphy
subject: Lake Pannon
subject: Hungary
subject: iron sulfide
subject: greigite
subject: endemic
subject: delta progradation
subject: EPOS
subject: multi-scale laboratories
subject: Paleomagnetic and magnetic data
subject: paleomagnetic data
subject (subjectScheme=EPOS WP16 Paleomagnetic Data Lithology): compound material > sedimentary material > carbonate sedimentary material > calcareous carbonate sedimentary material
subject (subjectScheme=EPOS WP16 Paleomagnetic Data Lithology): compound material > sedimentary material > clastic sedimentary material
subject (subjectScheme=EPOS WP16 Paleomagnetic Data Lithology): compound material > sedimentary material > sediment > mud size sediment > mud > clay
subject (subjectScheme=EPOS WP16 Paleomagnetic Data Lithology): compound material > sedimentary material > sediment > mud size sediment > mud > silt
subject (subjectScheme=EPOS WP16 Paleomagnetic Data Lithology): compound material > sedimentary material > sediment > sand size sediment > sand
subject (subjectScheme=EPOS WP16 Paleomagnetic Data Lithology): compound material > sedimentary material > sedimentary rock > generic mudstone > mudstone > shale
subject (subjectScheme=EPOS WP16 Paleomagnetic Data Lithology): compound material > sedimentary material > sedimentary rock > generic mudstone > mudstone > siltstone
subject (subjectScheme=EPOS WP16 Paleomagnetic Data Lithology): compound material > sedimentary material > sedimentary rock > organic rich sedimentary rock > coal > lignite
subject (subjectScheme=EPOS WP16 Paleomagnetic Data Location Type): Drill Site
CharacterString: Supplementary paleomagnetic data to: “Paleomagnetism in the Pannonian; Problems, Pitfalls, and Progress in using iron sulphides for magnetostratigraphy”
CharacterString: This dataset contains the paleomagnetic supplementary material to the article Kelder et al. (subm.), which presents a magnetostratigraphic correlation of Late Miocene lacustrine sediments based on multi-polarity greigite. The multi-polarity is visible in most thermal paleomagnetic results (Zijderveld diagrams) by antipodal high and medium temperature components, while only one magnetic component was visible in the alternating field demagnetization diagrams. Based on this complex behavior, a tailored demagnetization approach was developed to allow for reliable magnetostratigraphic dating of lacustrine sediments.
The dataset includes demagnetization data from four drill cores located nearby Paks, Hungary. They were not oriented, meaning that only the inclination could be used for paleomagnetism. The measurements took place at the Paleomagnetic Laboratory Fort Hoofddijk in Utrecht University, The Netherlands. For details about the methodology the reader is referred to the methodology in Kelder et al. (subm).
Three types of data are distinguished:
• Thermal demagnetization results (.th files)
• Alternating field demagnetization results (.af files).
• Interpreted magnetic vectors for demagnetization files (.dir files)
The .th, .af. and .dir files can be viewed with Notepad or similar programs, and analyzed via the Open Source platform Paleomagnetism.org (Koymans et al., 2016). The .dir files only exist for the cores PAET-30 and PAET-34, because these were interpreted in detail, while the material of the other cores (PAET-26, 27) were mainly used for rock magnetic purposes.
Finally, an overview of the data files, abbreviations and sample codes is provided in the data description file.
CharacterString: Data derive from four cores taken in the period 2015-2017
geographicElement
EX_GeographicBoundingBox
westBoundLongitude
Decimal: 18.6356
eastBoundLongitude
Decimal: 19.1299
southBoundLatitude
Decimal: 46.47
northBoundLatitude
Decimal: 46.7587
distributionInfo
MD_Distribution
transferOptions
MD_DigitalTransferOptions
onLine
CI_OnlineResource
linkage
URL: http://doi.org/10.5880/fidgeo.2018.007
protocol
CharacterString: WWW:LINK-1.0-http--link
name
CharacterString: Data Access - DOI
description
CharacterString: Data Access - DOI
function
CI_OnLineFunctionCode (codeList=http://www.isotc211.org/2005/resources/Codelist/gmxCodelists.xml#CI_OnLineFunctionCode codeListValue=http://www.isotc211.org/2005/resources/Codelist/gmxCodelists.xml#CI_OnLineFunctionCode_information): information
Released
Dataset
Abstract
;Utrecht University, The Netherlands
Files
