摘要
构造活动对成矿具有重要的控制作用,同位素年代学是厘定构造活动期次和成矿时代的重要手段。文章对近些年来同位素定年方法在这两方面所取得的进展进行了评述。
Structural activity is one of the important factors that control the formation of mineral deposits. Radiogenic isotopic chronological methods are used to precisely constrain the structural activities and mineralization epochs and have been developed rapidly. This paper briefly reviews the progress on tectono-thermal and mineralization geochronological methods and discusses their advantages and applicability.
出处
《地质找矿论丛》
CAS
CSCD
2008年第2期94-99,共6页
Contributions to Geology and Mineral Resources Research
基金
中国人民武装警察黄金部队项目"华熊地块构造-岩浆作用与金成矿的关系"
中国地质大学(北京)地质过程与矿产资源国家重点实验室科学基金(GPMR0734)联合资助
关键词
构造-热年代学
成矿年代学
研究进展
tectono-thermal geochronology
mineralization geochronology
research advance
