Contact metamorphic rocks of the studied area are composed of slates and hornfelses metamorphosed from the parts of Human and Jindong fromation by the intrusion of Hwawangsan granitic rocks. The contact aureole is divided into three zones from outermo...
Contact metamorphic rocks of the studied area are composed of slates and hornfelses metamorphosed from the parts of Human and Jindong fromation by the intrusion of Hwawangsan granitic rocks. The contact aureole is divided into three zones from outermost part to inner part, which indicate the albite-epidote hornfels facies, albite-epidote~hornblende hornfels transition facies, and hornblende hornfels facies.