Lithospheric structure beneath the ultra-slow spreading Knipovich ridge using noise reduced OBS P-wave Receiver functions ...

<!--!introduction!--> Ultra-slow spreading ridges are characterized by huge volcanic complexes which are separated by up to 150 km long amagmatic segments. The mechanisms controlling these types of mid-oceanic ridges (MOR) are not yet fully understood. We aim to constrain the crustal and mantl...

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Bibliographic Details
Main Authors: Rein, Theresa, Zahra, Zali, Frank, Krüger, Vera, Schlindwein
Format: Conference Object
Language:unknown
Published: GFZ German Research Centre for Geosciences 2023
Subjects:
Online Access:https://dx.doi.org/10.57757/iugg23-1638
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5017944