actinolitic greenschist facies的用法和样例：
- The Western Tianshan high-pressure metamorphic rocks occur within the greenschist facies country rocks as small discrete blocks, lenses, bands, laminae or intercalated slabs.
- All the rocks and strata in this zone are mylonitized and show steep foliation due to lower greenschist facies metamorphism and ductile strike-slip deformation.
- The retrograde metamorphism of the greenschist facies brittle ductile shear deformation and metamorphic zone,in conjunction with the brittle ductile,ductile brit...
- There are low-grade metamorphic rocks which underwent greenschist facies metamorphism in the middle and north margin of the Dabie ultrahigh pressure(UHP) metamorphic belt.