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The Xiaotian–Mozitan Shear Zone (XMSZ) is the boundary of the Dabie High‐grade Metamorphic Complex (DHMC) and the North Huaiyang Tectonic Belt. It was deformed in ductile conditions with a top‐to‐NW/WNW movement. Geothermometers applied to mineral parageneses in mylonites of the shear zone give a temperature range of 623–691°C for the predeformation and 515–568°C for the syndeformation, respectively,...
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