科迪勒拉型伸展与高温变质作用关系密切，伴随花岗质岩体的侵位，并使变质岩系近等温减压之后近等压冷却。
Cordillera type has a close relationship with high-temperature metamorphism and accompanied the emplacement of granitoid, giving rise to isothermal decompression and then isobaric cooling pT-t paths.
科迪勒拉型伸展与高温变质作用关系密切，伴随花岗质岩体的侵位，并使变质岩系近等温减压之后近等压冷却。
Cordillera type has a close relationship with high-temperature metamorphism and accompanied the emplacement of granitoid, giving rise to isothermal decompression and then isobaric cooling pT-t paths.
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