关于金伯利岩及其超基性岩包裹体中的铋在文献中没有任何报道。然而这些岩石又是地表上已知的最深物质,因而引起人们特别的注意。金伯利岩熔浆发育于地幔中,由于快速喷溢作用,看来受硅铝层的影响不大。超基性岩包裹体是金伯利岩岩浆在其上升时捕获来的上地幔岩石的捕虏体。在这些岩石中 Bismuth in kimberlites and their ultrabasic rock inclusions has not been reported in the literature. However, these rocks, again the deepest material known on the earth’s surface, have drawn special attention. The kimberlite melts develop in the mantle and appear to be less affected by the Si-Al layer due to the rapid jetting effect. Ultrabasic rock inclusions are the xenoliths of upper mantle rocks captured by kimberlite magma as it rises. Among these rocks