DIAMONDS FROM HIGH-PRESSURE METAMORPHIC ROCKS IN EASTERN DABIE MOUNTAIN

作     者：徐树桐 苏文 刘贻灿 江来利 季寿元 A.I.OKAY A.M.C.SENGOR 

作者机构：Anhui Institute of Geology Hefei 210001 PRC Department of Earth Science Nanjing University Nanjing 210008 PRC Department of Geology Istanbul Technical University Turkey (Department of Geology Istanbul Technical University Turkey 

出 版 物：《Chinese Science Bulletin》 (科学通报(英文版))

年 卷 期：1992年第37卷第2期

页      面：140-145页

核心收录：

学科分类：07[理学] 08[工学] 

基　　金：Project supported by the National Natural Science Foundation of China and Anhui Bureau of Geology and Minerol Resources 

主　　题：coesite jadeite diamond. 

摘      要：Diamonds commonly occur in kimberlites, lamproites and relative alluvial sediments. Some examples of diamonds discovered in ultramafics have heen reported. Sobolev and Shatsky reported diamonds from high-pressure metamorphic rock from northern Kazakhstan and considered it to be the source of the alluvial diamonds in Pridneprovie region of western U. S. S. R. Diamonds reported here show some similarity to those in northern Kazakhstan, and are the second occurrence in the world, but the first one in China.