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.
地壳中岩石的变形模式受构造应力、流体压力和上覆岩层重力共同作用的影响。
Deformation pattern of rocks in earth's crust is effected by tectonic stress, fluid pressure and gravity of the overlying strata.
盐上构造包括盐上滚动背斜、断弯-断展背斜、背冲断块、逆冲断层遮挡构造和盐推覆构造等；
The suprasalt structure includes suprasalt rolling anticline, fault-bending anticline, suprasalt pop-up, thrust screened structure and salt nappe.
形成这样的地质环境条件主要是岩浆侵入作用导致上覆火山岩的褶皱构造、侵入体的岩穹构造及接触破碎带构造等。
The geologic environment was mostly resulted from the intrusion of magma which led to folding of the overlying volcanic series, the formation of the intrusive dome and the contact broken zone.
窟窿山构造油藏目前是玉门油田的主力产油区块，也是增储上产最具潜力的区块，位于酒泉盆地青西凹陷南部，被祁连山北缘逆掩推覆。
Kulongshan Oil Reservoir, located in the south of the Qingxi Depression, Jiuxi Basin and overrided by the Qilianshan Mountain, is the primary producing area of the Yumen Oilfield.
富台油气田的主体构造由下古生界车古20潜山和其上覆的下第三系车3鼻状构造两部分组成。
The main structure of Futai oilfield is composed of the Lower Paleozoic Chegu 20 buried hill and the overlying Eogene Che 3 nose-like structure.
据深部资料结合区域地质特征分析，矿床为一滑覆构造系统。该系统上、下均有砂泥岩作屏蔽层，中间为云岩，形成一个对成矿极为有利的构造封闭系统。
According to regional geology and deep data, the deposit is considered as a gliding nappe system, whose upper and lower shielding layers are sandy mudstone, the middle part is dolomite.
据深部资料结合区域地质特征分析，矿床为一滑覆构造系统。该系统上、下均有砂泥岩作屏蔽层，中间为云岩，形成一个对成矿极为有利的构造封闭系统。
According to regional geology and deep data, the deposit is considered as a gliding nappe system, whose upper and lower shielding layers are sandy mudstone, the middle part is dolomite.
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