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新疆塔里木地台是我国古老稳定地台之一,1979年我们在该区工作时,发现了几处值得注意的岩石露头,1980年我们与局地矿处金庆民等怀疑其为金伯利岩,随采集了各种样品,经新疆地质局科研所马新兴、熊纪斌和周英森鉴定为金云母金伯利岩,新疆地质局实验室鉴定为超基性爆发角砾岩或角砾云母橄榄岩,后经地科院蒋荣、邓楚钧和赵春林复查后,认为此岩与金伯利岩一致。现就初步成果整理简介如下:
Tarim Basin in Xinjiang is one of the ancient stable platforms in our country. When we worked in this area in 1979, several notable rock outcrops were discovered. In 1980, we suspected it as kimberlite with the local mine, A variety of samples, the Xinjiang Geological Survey Ma Xinxing, Xiong Ji-Bin and Zhou Yingsen identified as gold mica kimberlite, Xinjiang Bureau of Geology laboratory identified as ultrabasic breccia or breccia mica peridotite, after the ASTRI Jiang Rong, Deng Chujun and Zhao Chunlin review, that this rock and kimberlite consistent. The preliminary results are summarized as follows: