thrust and nappe structures 逆冲推覆构造
The investigations show that the studied thrust-nappe structures began to form during the Devonian-Carboniferous periods,as a result of the southward Type A subduction zone is caused by collision of the Middle Kunlun Islands and the southern boundary of Tarim Block.
研究表明,铁克里克逆冲推覆构造是由于志留纪-泥盆纪古中昆仑岛弧与塔里木地体南缘的碰撞拼接作用,造成塔西南的南向A型俯冲,于泥盆纪-石炭纪开始发育形成的。
参考来源 - 塔西南铁克里克逆冲推覆构造的变形特征·2,447,543篇论文数据，部分数据来源于NoteExpress
The continental collision between Siberian and Kazakhstan-Junggar in Early Carboniferous shaped the large-scale dual thrust-nappe structures in the Altay orogen, NW China.
早石炭世末，准噶尔-哈萨克斯坦与西伯利亚板块发生陆-陆碰撞，形成大型双重逆冲推覆构造。
A variety of salt-related structures have developed in the Kuqa foreland fold-thrust belt, in which the most fascinating structure is the salt nappe complex.
盐岩层的存在使库车前陆褶皱-冲断带发育-系列盐相关构造，其中最引人注目的是盐推覆构造。
The over-thrust nappe in the margin of Daba Mountain is a zone with complex structures but fairly good prospects to hydrocarbon exploration.
大巴山前缘逆冲推覆带足一个构造复杂，但油气前景较好的地区。
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