thrusting-nappe fault 逆冲推覆断裂
They are fault metamorphic rocks formed in thrusting nappe structure inside continental plate during Variscan-Indonian Stage.
它们是华力西—印支期板内逆冲推覆构造所形成的断裂变质岩。
It is pointed out that the best gold metallogenic area are at uplifting and sagging edge of ductile complex fault of thrusting-nappe fault system.
提出逆冲体系中的韧脆性复成断裂带在带内的相对“上隆”和“下陷”的边缘地区以及其过渡带是金矿成矿的有利地区。
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