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）。
Various trap types have been formed in Tarim Basin during geological time. The two most important ones are drape anticline and block buried-hill trap types.
在塔里木盆地众多的圈闭类型中，中生界披覆背斜圈闭和以下古生界为主的断块潜山（或潜山）圈闭是最重要的两种高产圈闭型式。
Rock geochemistry displays an ocean island environment during the late sinian when the yili block broke away from the tarim plate.
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。
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