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...
मुख्य लेखकों: | Rees Jones, DW, Zhang, H, Katz, RF |
---|---|
स्वरूप: | Journal article |
भाषा: | English |
प्रकाशित: |
Royal Astronomical Society
2021
|
समान संसाधन
-
Consequences of glacial cycles for magmatism and carbon transport at mid-ocean ridges
द्वारा: Cerpa, N, और अन्य
प्रकाशित: (2019) -
Magmatic focusing to mid-ocean ridges: the role of grain size variability and non-Newtonian viscosity
द्वारा: Turner, AJ, और अन्य
प्रकाशित: (2017) -
Ridge migration, asthenospheric flow and the origin of magmatic segmentation in the global mid-ocean ridge system
द्वारा: Katz, R, और अन्य
प्रकाशित: (2004) -
Magma Dynamics with the Enthalpy Method: Benchmark Solutions and Magmatic Focusing at Mid-ocean Ridges
द्वारा: Katz, R
प्रकाशित: (2008) -
Magma dynamics with the Enthalpy Method: benchmark solutions and magmatic focusing at mid-ocean ridges
द्वारा: Katz, R
प्रकाशित: (2008)