摘要
<正>青藏高原是由高原上诸地块在不同时期碰撞-拼合到欧亚大陆南缘而形成的,其中羌塘地块与拉萨地块在侏罗-白垩纪的碰撞拼合导致班公湖-怒江中特提斯洋闭合,对青藏高原的早期形成和演化产生了巨大的影响。然而,不同学者通过不同研究方法对羌塘与拉萨地块碰撞拼合时限进行了探讨,但
引文
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