逆冲推覆构造由推覆体系、前缘带、前缘外带和原地岩体四部分组成的。
The over thrust nappe consists of four parts: nappe system, front zone, outer front zone and autochthon.
从胡家营的推覆构造可推知汉南地块东南缘北东向构造带，应属于中生代以来所形成的推覆体构造。
It is supposed that the NE structural belt along southeast margin of Hannan Massif belongs to the nappe formed after Mesozoic Era in terms of Hujiaying nappe.
本文用被动顶板双重构造模式来解释该推覆体群的运动学模式，并据该区的地质特征对经典的被动顶板双重构造模式进行了补充。
The authors explain its kinematic model with the passive roof duplex and enrich the classical passive roof duplex according to the geological features of this area.
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