Zobrazeno 1 - 4
of 4
pro vyhledávání: '"L. E. R. Pedersen"'
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 25, Iss 4, Pp n/a-n/a (2024)
Abstract The ultraslow‐spreading Mohns Ridge is a key supersegment of the Arctic Mid‐Ocean system, where it represents a boundary between the Jan Mayen hotspot in the south and the highly anomalous Knipovich Ridge to the north. Understanding the
Externí odkaz:
https://doaj.org/article/99d20c690c2249ac89b69e6dd829b894
Publikováno v:
Nature Communications, Vol 14, Iss 1, Pp 1-8 (2023)
Abstract Nearly 30% of ocean crust forms at mid-ocean ridges where the spreading rate is less than 20 mm per year. According to the seafloor spreading paradigm, oceanic crust forms along a narrow axial zone and is transported away from the rift valle
Externí odkaz:
https://doaj.org/article/e5939a2e63f541b98e13ef2d14380464
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 23, Iss 11, Pp n/a-n/a (2022)
Abstract The Mohns Ridge is a very slow‐spreading ridge that, together with the Knipovich Ridge, marks the boundary between the North American and Eurasian plates in the Norwegian‐Greenland Sea. In this study, we report the major and trace elemen
Externí odkaz:
https://doaj.org/article/3451b2fa4d3b4f09894a9b9baeb349a4
Publikováno v:
European Journal of Mineralogy, Vol 35, Pp 969-985 (2023)
Central Dronning Maud Land (cDML) is part of the late Mesoproterozoic Maud Belt in East Antarctica, which was metamorphosed and deformed during the Ediacaran–Cambrian Gondwana assembly. Here we study high-pressure (HP) mafic rocks in Gjelsvikfjella
Externí odkaz:
https://doaj.org/article/3a7a16a79c91497b95350e032ff582ba