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زمینشناسی و معدن::
صفحه فرورانش شده
The oceanic part of the subducting plate tears off and continues to drop down, a process referred to as "slab breakoff ".
Low temperatures in the crust are caused by the coolness of the subducting plate underneath and prevent the formation of magma by melting or the rise of magma from deeper sources.
Subduction zones can be subdivided into two types, based on characteristics of the subducted plate (Uyeda and Kanamori, 1979).
, towards the subducting plate or easterly into the edge of the Pacific Plate in the case of the Marianas.
The subducting plate is intermittently coupled to the upper plate because of the buoyancy of the former; this causes compression and thickening of the upper plate (Fig. 7.5).
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