陆内碰撞体制流体作用及成矿作用研究的意义和现状  

SIGNIFICANCE AND CURRENT SITUATION OF STUDY ON FLUIDIZATION AND MINERALIZATION UNDER INTRACONTINENTAL COLLISION REGIME

作　　者：陈衍景[1] 于方[1] 魏绮英 高秀丽[1] 常兆山[1] 宋新宇[1] 

机构地区：[1]北京大学地质系

出　　处：《地球科学进展》1995年第4期318-322,共5页Advances in Earth Science

摘　　要：陆内碰撞作用和流体作用都是８０年代以来的研究前沿，它们的研究必然会大大促进成矿作用研究的发展，也是跟踪和超越世界地球科学先进水平的重要途径。中国拥有最多最复杂的陆内碰撞带，为中国学者开展有关研究并取得高水平成果提供了得天独厚的条件。对陆内碰撞、流体作用和成矿作用研究现状的分析表明，三者之间研究的相互结合是薄弱环节，限制了有关问题的深入，但为我国学者开展该方向的研究，取得领先于国际水平的成果，提供了十分难得的良好时机。Since 1980s,both intracontinental collision and fluidization have become the forwardresearch fields,The upsurge and progress in these two research fields must lead to a greatimprovement in study of metallogenesis. Therefore, comprehensive study of collision, flu-idization and mineralization will be taken on the forward trends of sciences;and it is also amost important way to trace or get ahead of the international progress in Earth sciences. Intracontinental collision orogenic belts are most universal and most complex in China,which provides unique conditions for Chinese geologists to take researching work and toget ahead knowledge on subjects related to collision orogenesis. Reviews of the current research stage of intracontinental collision ,fluidization andmineralization shows that comprehensive study of these three fields is still absent.And theabsence will forbid further insighting in related problems. But it provides a rare chance forChinese scientists to study and to obtain forward understanding in the research direction.Therefore,the authors appeal to initiate studying in the direction as soon as possible.

关 键 词：陆内碰撞 流体作用 成矿作用 

分 类 号：P612[天文地球—矿床学]