该文认为,阿尔金山走滑断裂构造是一巨型左行左列走滑断裂兼逆冲推覆和韧性剪切性质的断裂构造带。
This paper considers that Aerjin Mountain strike-slip fault structure is a huge tectonic zone with the property of left active anticlockwise and thrust nappes and ductile shear zone.
晚白垩世早第三纪郯庐断裂带转变成巨型的伸展构造,普遍控制发育了断陷盆地。
The Tan Lu fault zone turned into a huge extensional structure during Late Cretaceous to Eogene, leading to a series of development of fault bounded basins.
湖北谷城县观音坪地区推覆构造为武当山巨型推覆构造的一部分。
Decollement-nappe structure of the Guanyinping region is a part of nappe structure of Wudang Mountain.
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