在大洋板块与大陆板块的碰撞地带 ,通常伴有规模较大的成矿作用 ,这是地质学界公认的规律之一。但青藏高原的快速隆升是由于印度板块与亚洲板块两大陆之间的碰撞 ,其主隆升段大约仅为 2 0 0 0万年到 1 40 0万年前 ,抬升规模较大 ,并在抬升的过程中不断剥蚀矿物质。因此 ,多数地 In the collision zone between the oceanic plate and the continental plate, it is usually accompanied by a large-scale mineralization, which is one of the accepted laws in geology. However, the rapid uplift of the Qinghai-Tibet Plateau is due to the collision between the Indian and Asian plates, with the main uplift only about 20 to 40 million years ago, with a large uplift and at The process of lifting the continuous erosion of minerals. Therefore, most of them