thrusting-nappe fault 逆冲推覆断裂
thrusting nappe fault 逆冲推覆断裂
thrusting nappe structure 逆冲推覆构造
thrusting-nappe structures 逆冲推覆构造
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。
The Ruzhou coalfield lies at the front part of thrusting nappe structural zone western Henan sector, south margin of the North China plate.
汝州煤田位于华北板块南缘逆冲推覆构造带豫西段前锋部位，区内逆冲推覆构造较发育。
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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