To understand subduction initiation, study forearc crust: To understand forearc crust, study ophiolites
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چکیده
منابع مشابه
Mantle hydration and Cl-rich fluids in the subduction forearc
In the forearc region, aqueous fluids are released from the subducting slab at a rate depending on its thermal state. Escaping fluids tend to rise vertically unless they meet permeability barriers such as the deformed plate interface or the Moho of the overriding plate. Channeling of fluids along the plate interface and Moho may result in fluid overpressure in the oceanic crust, precipitation o...
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Formation of forearc basins and their influence on subduction zone earthquakes
Recent observations of an association between forearc basins and slip during subduction thrust earthquakes suggest a link between processes controlling upper plate structure and seismic coupling on the subduction-zone thrust fault. We present a mechanism for the formation of these basins where sedimentation occurs on landward-dipping segments of the subduction wedge, which itself is actively gr...
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متن کاملSubduction-RelatedMagmatic Arcs, with an Emphasison Primitive Andesiteand Lower Crust
3.18.3 CHARACTERISTICS OF ARC MAGMAS 7 3.18.3.1 Comparison with MORBs 7 3.18.3.1.1 Major elements 7 3.18.3.1.2 We are cautious about fractionation correction of major elements 9 3.18.3.1.3 Distinctive, primitive andesites 11 3.18.3.1.4 Major elements in calc-alkaline batholiths 11 3.18.3.2 Major and Trace-Element Characteristics of Primitive Arc Magmas 18 3.18.3.2.1 Primitive basalts predominat...
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ژورنال
عنوان ژورنال: Lithosphere
سال: 2012
ISSN: 1947-4253,1941-8264
DOI: 10.1130/l183.1