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An X-Ray Diffraction Study of an Inclusion in Diamond from the Luobusha Chromite Deposit in Tibet,China 被引量:1
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作者 SHINicheng BAIWenji +5 位作者 MAZhesheng FANGQingsong XIONGMing YANBinggang daimingquan YANGJingsui 《Acta Geologica Sinica(English Edition)》 SCIE CAS CSCD 2003年第3期326-331,共6页
Diamond was found in podiform chromitites of ophiolite and harzburgite from Luobusha, Tibet. There are silicate inclusions in some diamond grains from this area. In the present work, the CCD (charge coupled detector) ... Diamond was found in podiform chromitites of ophiolite and harzburgite from Luobusha, Tibet. There are silicate inclusions in some diamond grains from this area. In the present work, the CCD (charge coupled detector) technology of X-ray powder diffraction was applied to the study of the inclusion in diamond from the ophiolite of Tibet. Diffraction patterns are obtained even though the inclusion is only 20 μm in crystal size. The results show that the inclusion in diamond consists of talc and clinochrysotile. Therefore, it is clear that the diamond from the ophiolite of Luobusha, Tibet, is natural diamond rather than a synthetic one. 展开更多
关键词 diamond from ophiolite inclusion in diamond Luobusha of Tibet China
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