The authors put forward that Daba-Xiugugabu Ophiolite belt originated from an ancient oceanic crust fragment of India continental northern marginal ocean basin, that was approximately synchronous with the formation and evolution period of the Neo-Tethys o
The authors put forward that Daba-Xiugugabu Ophiolite belt originated from an ancient oceanic crust fragment of India continental northern marginal ocean basin, that was approximately synchronous with the formation and evolution period of the Neo-Tethys o
笔者提出该区蛇绿岩来源于印度大陆北缘洋盆的洋壳碎片，这个陆缘洋盆与新特提斯洋主体的形成和演化准同步。