Subduction‐Induced Upwelling of a Hydrous Transition Zone: Implications for the Cenozoic Magmatism in Northeast China
Volume: 124, Issue: 11, Pages: 11489 - 11504
Published: Nov 1, 2019
Abstract
The widespread Cenozoic basalts in northeast China are commonly thought to be related to the stagnation of the Pacific slab in the transition zone and its deep dehydration. By incorporating experimentally constrained phase diagrams of hydrous mantle and melting conditions at high pressures into two‐dimensional petrological‐thermomechanical models, here we model the interaction of a subducting slab with a hydrous transition zone (TZ) and examine...
Paper Details
Title
Subduction‐Induced Upwelling of a Hydrous Transition Zone: Implications for the Cenozoic Magmatism in Northeast China
Published Date
Nov 1, 2019
Volume
124
Issue
11
Pages
11489 - 11504
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