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;
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