Sublithospheric small-scale convection—A mechanism for collision zone magmatism
نویسندگان
چکیده
منابع مشابه
On the state of sublithospheric upper mantle beneath a supercontinent
S U M M A R Y An assumption of isothermal and static asthenosphere as the normal state of sublithospheric mantle, as commonly employed in studies of terrestrial magmatism, may be physically implausible for a system cooled from above. The growth of an unstable thermal boundary layer at the base of the lithosphere can lead to small-scale convection, so asthenosphere is expected to be usually conv...
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ژورنال
عنوان ژورنال: Geology
سال: 2014
ISSN: 1943-2682,0091-7613
DOI: 10.1130/g35193.1