Volatiles beneath mid-ocean ridges: Deep melting, channelised transport, focusing, and metasomatism
نویسندگان
چکیده
منابع مشابه
A Self-Consistent Model of Melting, Magma Migration and Buoyancy-Driven Circulation Beneath Mid-Ocean Ridges
Numerical modeling and anMysis are used to investigate the processes leading to the eruption of mantle-derived magma at mid-ocean ridges. Our model includes the following effects: melting due to decompression, magma migration by percolation, and circulation of the mantle driven by both the oceanic plates and the distribution of buoyancy beneath the ridge. The distribution of buoyancy is due to ...
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ژورنال
عنوان ژورنال: Earth and Planetary Science Letters
سال: 2017
ISSN: 0012-821X
DOI: 10.1016/j.epsl.2017.02.006