该裂谷为塔里木南缘晚古生代活动带的一部分。
The rift is a part of the late Paleozoic active belt in the margin of Tarim.
塔里木南缘中部存在一显著的低速区，可能与岩浆活动和构造活动较强有关。
A definite low Pn velocity region to the south of Tarim basin is possibly related to strong magma and tectonic activity.
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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