Reply to comment by Qi and Wang on “Similar crust beneath disrupted and intact cratons: Arguments against lower-crust delamination as a decratonization trigger”
Tectonophysics(2019)
摘要
•Their discussion was based on misinterpretation of our data.•Their comments do not alter our original interpretation.•Both crust beneath disrupted and intact parts of the craton are low-Vp and andesitic.
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