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1·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。

2·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；

3·The Tarim basin was formed under control of the continental contage of Tarim block in Paleo-Asia continent and the open of Paleo-Tethys ocean. And rifting belt was formed in Tienshan-Jihei(C1-P1);

塔里木地块在北部古亚洲大陆拼贴和南部古特提洋打开影响下形成盆地，从天山到吉黑形成一系列的裂谷带（C1—P1）。