自七十年代初期板块构造学说引进我国后,蛇绿岩的研究逐渐引起我国地学界的重视。特别是在空间、时间上,蛇绿岩在我国有着广袤、多期的分布特征,近几年来在科研工作中、区域地质调查及普查找矿中,较普遍地开展了蛇绿岩的研究。1981年和1982年分别在西安、沈阳召开了有关蛇绿岩和板块构造及其成矿关系的会议;与会代表来自祖国各方,他们从不同地学专业,提出了具一定水平的论述,为今后进一步开展工作,提供了大量有价值的资料。 Since the introduction of the tectonic theory of plate tectonics in the early 1970s, the research on ophiolite gradually attracted the attention of geosciences in China. Especially in space and time, ophiolite has a vast and multi-period distribution in our country. In recent years, ophiolite has been studied in scientific research, regional geological survey and prospecting. In 1981 and 1982, respectively, held in Xi’an, Shenyang, ophiolite and plate tectonics and mineralization relations meeting; delegates from all walks of life, they from different geography, put forward a certain level of discussion for the future Further work, provided a lot of valuable information.