Temperature-increase metamorphism along the south boundary of the Dabie eclogite terrain, China.
大别山太湖—马庙断裂带两侧变质地体的增温变质作用

The south boundary of the Dabie eclogite terrain extends west east along Taihu Mamiao faults zone with a south dip Both eclogite and amphibolite along the south of the boundary experienced a temperature increasing and pressure decreasing metamorphic