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Melt Evolution above a Spontaneously Retreating Subducting Slab in a Three-Dimensional Model

Zhu, Guizhi ; Gerya, Taras ; Yuen, David A.

Journal of earth science (Wuhan, China), 2011-04, Vol.22 (2), p.137-142 [Periódico revisado por pares]

China University of Geosciences: China University of Geosciences

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Título:
Melt Evolution above a Spontaneously Retreating Subducting Slab in a Three-Dimensional Model
Autor: Zhu, Guizhi ; Gerya, Taras ; Yuen, David A.
Assuntos: Biogeosciences ; Computational fluid dynamics ; Dehydration ; Earth and Environmental Science ; Earth science ; Earth Sciences ; Evolution ; Evolutionary biology ; Geochemistry ; Geology ; Geotechnical Engineering & Applied Earth Sciences ; Melting ; Melts ; Moisture content ; Rocks ; Slabs ; Volcanoes ; 三维模型 ; 俯冲板块 ; 俯冲板片 ; 地幔熔融 ; 容积率 ; 极大值 ; 水分含量 ; 熔体演化
É parte de: Journal of earth science (Wuhan, China), 2011-04, Vol.22 (2), p.137-142
Notas: TP391.41
subduction, water and melt, three-dimensional model.
42-1788/P
P541
ObjectType-Article-1
SourceType-Scholarly Journals-1
ObjectType-Feature-2
content type line 23
Descrição: Dehydration of the subducting slab favors the melting of the surrounding mantle. Water content and melt evolution atop a spontaneously retreating subducting slab are reported in a three- dimensional （3-D） model. We find that fluids, including water and melts in the rocks, vary substantially along the trench, which cannot be found in two-dimensional （2-D） models. Their maxima along the subducting slab are mainly located at about 50 to 70 and 120 to 140 kin. Volumetric melt production rate changes spatially and episodically atop the slab, which may reflect the intensity and variations of volcanoes.
Editor: China University of Geosciences: China University of Geosciences
Idioma: Chinês;Inglês

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Melt Evolution above a Spontaneously Retreating Subducting Slab in a Three-Dimensional Model

Zhu, Guizhi ; Gerya, Taras ; Yuen, David A.

China University of Geosciences: China University of Geosciences

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