Ultraslow spreading ridges form the slowest divergent plate boundaries and exhibit distinct spreading processes in volcanically active magmatic sections and intervening amagmatic sections. Local seismicity studies of ultraslow spreading ridges until now cover only parts of segments and give insight...
Bibliographic Details
Published in: | Geochemistry, Geophysics, Geosystems |
Main Authors: |
Meier, Michaela,
Schlindwein, Vera,
Scholz, John‐Robert,
Geils, Jonah,
Schmidt‐Aursch, Mechita C.,
Krüger, Frank,
Czuba, Wojciech,
Janik, Tomasz,
Schlindwein, Vera; 1 Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research Bremerhaven Germany,
Scholz, John‐Robert; 1 Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research Bremerhaven Germany,
Geils, Jonah; 1 Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research Bremerhaven Germany,
Schmidt‐Aursch, Mechita C.; 1 Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research Bremerhaven Germany,
Krüger, Frank; 3 Institute for Geosciences University of Potsdam Potsdam Germany,
Czuba, Wojciech; 4 Institute of Geophysics Polish Academy of Sciences Warszawa Poland,
Janik, Tomasz; 4 Institute of Geophysics Polish Academy of Sciences Warszawa Poland |
Format: | Article in Journal/Newspaper
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Language: | English |
Published: |
2021
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Subjects: |
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Online Access: | https://doi.org/10.23689/fidgeo-4322
http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/8668
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