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.
培面出露较好，岩石化学、地球化学特征显示为大洋岛屿环境，是震旦纪晚期伊犁地块从塔里木板块裂解时的产物。
Rock geochemistry displays an ocean island environment during the late sinian when the yili block broke away from the tarim plate.
塔里木克拉通由塔北地块与塔南地块晋宁运动时拼合形成，基底构造线因地而异。
The Tarim Craton was created in the Jinningian orogeny by amalgamation of the North Tarim and South Tarim Blocks, with the basement structures being varied in its northern, middle and southern parts.
塔里木克拉通由塔北地块与塔南地块晋宁运动时拼合形成，基底构造线因地而异。
The Tarim Craton was created in the Jinningian orogeny by amalgamation of the North Tarim and South Tarim Blocks, with the basement structures being varied in its northern, middle and southern parts.
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