,Explosion of Ultrahigh Pressure Minerals in Mantle

• 作 者: BAI Wenji YANG Jingsui FANG Qingsong YAN Binggang ZHANG Zhongming
• 机 构: Institute of Geology, Chinese Academy of Geological Sciences, 100037
• 出 处: 大陆动力学（英文版）
• 发表日期: 2001年2期

The microexplosion stucture of ultrahigh pressure minerals was found for the first time in podform chromitites within the mantle peridotite facies of Luobusa ophiolite along the Yarlung Zangbo suture zone.The explosion stuctures of high-energy silicate inclusions are commonly seen in thin sections (see figure).