印度次大陆从南极洲脱离，漂过印度洋越过喜马拉雅山与亚洲陆块猛烈碰撞；
The Indian subcontinent detaching itself from Antarctica and sweeping across the Indian Ocean to its violent collision with Asia's landmass across the Himalayas;
该构造带的发现支持了古亚洲构造域对东北微陆块区的影响一直延续到中侏罗世的观点。
The discovery of this tectonic zone supports the view that the influence of the Paleo-Asiatic tectonic domain on the Northeast China microblock persisted till the Middle Jurassic.
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