Magmatic channelization by reactive and shear-driven instabilities at mid-ocean ridges: a combined analysis

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...

Cur síos iomlán

Sonraí bibleagrafaíochta
Príomhchruthaitheoirí:	Rees Jones, DW, Zhang, H, Katz, RF
Formáid:	Journal article
Teanga:	English
Foilsithe / Cruthaithe:	Royal Astronomical Society 2021

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