幔源岩浆的底侵及软流圈对地壳的直接加热作用，使上覆地壳发生大规模的岩浆和成矿作用，并导致中国东部中生代时期伸展构造的广泛发育。
The heating from the asthenosphere on the crust subsequently resulted in the intensive magmatism, mineralization, and widespread development of extensional structures in eastern China.
北部“明龙山—上窑构造带” ，是位于淮南煤田北缘由北向南逆冲的推覆构造带；
Minglongshan-Shangyao structural belt in north is other over-thrust belt with N-S direction.
该文在简述推覆构造阵列主要类型的基础上，介绍了新疆北山地区鳞片叠覆推覆构造的基本特征。
Based on the summarization of the main types of nappe structure array, this article discusses the main features of the Beishan scaly imbrication nappe structure in Xinjiang.
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