塔里木地块和柴达木地体的古地磁数据表明，阿尔金断裂至少经历了四期活动。
The paleomagnetic results of Tarim and Qaidam indicate that Altyn Taugh fault has experienced complicated tectonic activity.
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）。
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);
铁克里克古陆缘地块位于塔里木盆地之西南缘。
Ancient land reason massif crick of iron lie in southwest predestination of tarim basin.
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