出露于柴达木盆地北缘加里东裂谷带东段托莫尔日特地区的一套酷似蛇绿岩的岩石组合 ,其地质、地球化学特征显示它们并不具备洋壳性质 ,而应为形成于陆壳内的 ,即没有洋壳出现的陆缘裂谷环境下的一种似蛇绿岩组合。提出了与蛇绿岩不同的动力学形成模式 ,所讨论的似蛇绿岩可能是并无洋壳出现的陆缘裂谷的较典型代表。 A suite of rock-like ophiolite-like assemblages exposed in the Tomorite area east of the Caledonian rift zone on the northern margin of the Qaidam basin have geologic and geochemical characteristics that indicate that they do not possess oceanic crustal properties It is an ophiolite-like assemblage formed in the continental crust, ie, in a continental rifting environment where no oceanic crust appears. Proposed a different kinetic formation model than ophiolite. The ophiolite discussed here may be the representative representative of continental rifting that does not occur in the oceanic crust.