摘要
采用空间分辨率高和高灵敏度的质子微探针和微束PIXE技术,测定地幔流体结晶后各组成矿物的微量元素组成及其在不同矿物内的分布状况。对云南双沟蛇绿岩中存在的地幔交代作用进行的研究结果表明,由地幔流体结晶而成的矿物(单斜辉石、尖晶石、石榴石、绿泥石),其微量元素组成与分布特征受地幔交代作用过程的控制。
A study on trace element composition and distribution in minerals crystallized from mantle fluids based on the phenomenon of metasomatism in the Shuanggou ophiolite is reported in this paper. Proton microprobe and micro PIXE technique with high spatial resolution and high detection sensitivity are used in the study. The results indicate that trace element compositon and distribution in minerals(monoclinic pyroxene, spinel, garnet and chlorite) crystallized from mantle fluids are controlled by mantle metasomatism processes. It is of great importance in further study of the geochemical behavior of trace elements in the Shuanggou mantle metasomatism processes.
出处
《岩矿测试》
CAS
CSCD
北大核心
1996年第3期168-172,共5页
Rock and Mineral Analysis
基金
国家自然科学基金
中国科学院核分析技术开放实验室共同资助
关键词
蛇绿岩
地幔
交代作用
质子微探针
the Shuanggou ophiolite, metasomatism, proton microprobe, micro proton induced X ray emission(μ PIXE), trace element, composition and distribution