Contrasting spreading processes at Gakkel Ridge across the 3°E boundary shaped the Arctic Ocean lithosphere

The Arctic mid-ocean ridge system is one of the two main representatives of the particular class of ultraslow spreading ridges with spreading rates of less than 20 mm/y full rate. The formation of new ocean lithosphere at these ridges strongly deviates from any other ocean basin. Typical properties...

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Bibliographic Details
Main Authors: Schlindwein, Vera, Schmid, Florian
Format: Conference Object
Language:unknown
Published: 2015
Subjects:
Online Access:https://epic.awi.de/id/eprint/38193/
https://epic.awi.de/id/eprint/38193/1/abstract_icam_2015_schlindwein.pdf
https://hdl.handle.net/10013/epic.45649
https://hdl.handle.net/10013/epic.45649.d001