Magmatic channelization by reactive and shear-driven instabilities at mid-ocean ridges: a combined analysis
It is generally accepted that melt extraction from the mantle at mid-ocean ridges (MORs) is concentrated in narrow regions of elevated melt fraction called channels. Two feedback mechanisms have been proposed to explain why these channels grow by linear instability: shear flow of the partially molte...
Autors principals: | Rees Jones, DW, Zhang, H, Katz, RF |
---|---|
Format: | Journal article |
Idioma: | English |
Publicat: |
Royal Astronomical Society
2021
|
Ítems similars
-
Consequences of glacial cycles for magmatism and carbon transport at mid-ocean ridges
per: Cerpa, N, et al.
Publicat: (2019) -
Magmatic focusing to mid-ocean ridges: the role of grain size variability and non-Newtonian viscosity
per: Turner, AJ, et al.
Publicat: (2017) -
Ridge migration, asthenospheric flow and the origin of magmatic segmentation in the global mid-ocean ridge system
per: Katz, R, et al.
Publicat: (2004) -
Magma Dynamics with the Enthalpy Method: Benchmark Solutions and Magmatic Focusing at Mid-ocean Ridges
per: Katz, R
Publicat: (2008) -
Magma dynamics with the Enthalpy Method: benchmark solutions and magmatic focusing at mid-ocean ridges
per: Katz, R
Publicat: (2008)