摘要
In this paper, the authors report two cases of lamellea (in scales of 1 μm and over 100 μm seperately) olivines in mantle xenoliths from the Halaha River and Chaoer River area, Central Great Xing’an Range. The results of EMP analysis indicate that the lamellae is Fe rich olivine. In response to the arguments against the hypothesis of exsolution and erosion, the authors discuss the behavior and mechanism of Cottrell cloud in olivine.