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Polyphase Magmatism During the Formation of the Northern East Greenland Continental Margin

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Dokumenter

DOI

  • D. Franke, Federal Institute for Geosciences and Natural Resources
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  • P. Klitzke, Federal Institute for Geosciences and Natural Resources
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  • U. Barckhausen, Federal Institute for Geosciences and Natural Resources
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  • K. Berglar, Federal Institute for Geosciences and Natural Resources
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  • C. Berndt, Helmholtz Centre for Ocean Research Kiel
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  • V. Damm, Federal Institute for Geosciences and Natural Resources
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  • A. Dannowski, Helmholtz Centre for Ocean Research Kiel
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  • A. Ehrhardt, Federal Institute for Geosciences and Natural Resources
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  • M. Engels, Federal Institute for Geosciences and Natural Resources
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  • T. Funck, Geological Survey of Denmark and Greenland
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  • W. Geissler, Alfred Wegener Institute - Helmholtz Centre for Polar and Marine Research
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  • M. Schnabel, Federal Institute for Geosciences and Natural Resources
  • ,
  • M. Thorwart, Christian-Albrechts-Universität zu Kiel
  • ,
  • Per Trinhammer

New marine geophysical data acquired across the partly ice-covered northern East Greenland continental margin highlight a complex interaction between tectonic and magmatic events. Breakup-related lava flows are imaged in reflection seismic data as seaward dipping reflectors, which are found to decrease in size both northward and southward from a central point at 75°N. We provide evidence that the magnetic anomaly pattern in the shelf area is related to volcanic phases and not to the presence of oceanic crust. The remnant magnetization of the individual lava flows is used to deduce a relative timing of the emplacement of the volcanic wedges. We find that the seaward dipping reflectors have been emplaced over a period of 2–4 Ma progressively from north to south and from landward to seaward. The new data indicate a major post-middle Eocene magmatic phase around the landward termination of the West Jan Mayen Fracture Zone. This post-40-Ma volcanism likely was associated with the progressive separation of the Jan Mayen microcontinent from East Greenland. The breakup of the Greenland Sea started at several isolated seafloor spreading cells whose location was controlled by rift structures and led to the present-day segmentation of the margin. The original rift basins were subsequently connected by steady-state seafloor spreading that propagated southward, from the Greenland Fracture Zone to the Jan Mayen Fracture Zone.

OriginalsprogEngelsk
TidsskriftTectonics
Vol/bind38
Nummer8
Sider (fra-til)2961-2982
Antal sider22
ISSN0278-7407
DOI
StatusUdgivet - aug. 2019

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