Experimental evidence supports mantle partial melting in the asthenosphere
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چکیده
منابع مشابه
Experimental evidence supports mantle partial melting in the asthenosphere
The low-velocity zone (LVZ) is a persistent seismic feature in a broad range of geological contexts. It coincides in depth with the asthenosphere, a mantle region of lowered viscosity that may be essential to enabling plate motions. The LVZ has been proposed to originate from either partial melting or a change in the rheological properties of solid mantle minerals. The two scenarios imply drast...
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ژورنال
عنوان ژورنال: Science Advances
سال: 2016
ISSN: 2375-2548
DOI: 10.1126/sciadv.1600246