ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
橄榄石的后尖晶石相变研究进展
  
关键词:olivine  post-spinel phase transformation  advance
基金项目:国家自然科学基金项目(编号:40402006),教育部高等学校优秀青年教师教学和科研奖励计划
作者单位E-mail
翟双猛 中国科学院广州地球化学研究所510640 shm-zhai@sohu.com 
夏斌 中国科学院广州地球化学研究所510640  
陈汉林 浙江大学理学院地球科学系杭州310027  
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摘要:
Advances in the Study of Post-Spinel Phase Transformation of Olivine
      Ringwoodite, one of the high-pressure and high-temperature forms of olivine, can be decomposed into perovskite and periclase (post-spinel phase transformation). The process, which seems to be one of the most important transformations in the Earth′s mantle, is believed to be the cause of the 660-km seismic discontinuity dividing the mantle into upper and lower parts. The advances made in the researches are shown in three aspects: ① post-spinel phase transformation of Mg_2SiO_4 at high pressure and high temperature using in situ X-ray diffraction; ② the effects of H_2O, Al_2O_3 and equation of state of gold on the post-spinel phase transformation; ③ the post-spinel phase transformation in peridotite under lower mantle conditions. On the basis of a summary of recent advances, this paper analyzes the existing problems and indicates possible directions for further studies.
ZHAI Shuang-meng,XIA Bin,CHEN Han-lin.2006.Advances in the Study of Post-Spinel Phase Transformation of Olivine[J].Acta Geoscientica Sinica,27(1):75-79.
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