The North China continental block and the Yangtze continental block are separated by the Xiangshuikou-Qianliyan deep fracture.
华北陆块与扬子陆块以响水口一千里岩深断裂为界。
These patterns of extensional structures suggested that deformations of the Qinling continental block with special continental dynamics had been undergone shearing extension.
这些伸展构造样式显示秦岭微板块是以伸展作用发生陆壳变形的，可称为秦岭型伸展构造样式；
These patterns of extensional structures suggested that deformations of the Qinling continental block with special continental dynamics had been undergone shearing extension.
这些伸展构造样式显示秦岭微板块是以伸展作用发生陆壳变形的，可称为秦岭型伸展构造样式；
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