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
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