The researches show that the Neo tectonic activity of Xinjiang is not the simple reactivation of an ancient plate.
研究结果表明，新疆新构造运动不是古板块的简单复活。
The plate collision helped close the western part of the ancient Tethys Sea and lifted up the massive European mountain chain that persists today.
同时，这次板块碰撞封闭了特提斯海(即古地中海)的西部，并且形成了仍保存至今的欧洲大部分山脉。
The major disruption of Heigou-Luanchuan has determined the active continental margin of the ancient north China plate.
黑沟一栾川大断裂，限定了古华北板块南部活动大陆边缘的边界。
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