北京昌平地区串岭沟组沉积岩中独居石、金红石赋存状态及其成因  

Occurrence and Origin of Monazites and Rutiles from Sedimentary Rocks of Chuanlinggou Formation in Changping Area of Beijing

作　　者：丁静[1,2] 宋天锐[3] 石玉若[2] 

机构地区：[1]中国地质大学(北京)研究生院,北京100083 [2]中国地质科学院地质研究所北京离子探针中心,北京100037 [3]中国地质科学院地质研究所,北京100037

出　　处：《地球科学与环境学报》2016年第2期172-181,共10页Journal of Earth Sciences and Environment

基　　金：国家自然科学基金项目(41173065);国土资源部公益性行业科研专项经费项目(201311116);中国地质科学院地质研究所基本科研业务费项目(J1403)

摘　　要：对采自北京昌平地区串岭沟组下部层位粉砂质泥岩中的矿物进行了详细的能谱分析,发现了独居石和金红石颗粒。独居石最大粒径为88μm,金红石最大粒径为20μm。背散射图像显示独居石边缘不平整,形状不规则,呈现出"鱼形"、"鸟形"、"花形"、"虫形"等各种形状;金红石则呈串珠状分布。大量的观察发现,独居石和金红石绝大多数都分布在石英脉或赤铁矿细脉里,远离脉的地方几乎没有独居石和金红石的分布。独居石初步SHRIMP U-Pb原位定年结果为(152±11)Ma,表明这些独居石颗粒并非成岩期形成,而为次生独居石,其形成与后期的热液事件有关。Monazite and rutile grains are found in the contribution by using energy spectrum analysis to study the silty mudstones,which are collected from the lower part of Chuanlinggou Formation in Changping area of Beijing.The maximum particle size of the monazite is up to 88μm while the largest rutile is 20μm.According to lots of backscattered images,the monazites show jagged edges and irregular shapes,appeared as fishes,birds,flowers,worms,and so on,while the rutiles are arranged as a string of beads.An overwhelming majority of the monazites and rutiles are distributed in quartz or hematite veins.However,monazites or rutiles are hardly found in the places far away from the veins.These monazites with the age of（152±11）Ma are dated using SHRIMP Ⅱ at Beijing SHRIMP Center.According to the preliminary age data,it is suggested that these monazites belong to secondary monazites,which are associated with the late hydrothermal event,not formed in the diagenetic stage.

关 键 词：成因矿物学 串岭沟组 独居石 金红石 热液成因 SHRIMP U-PB年龄 能谱分析 北京 

分 类 号：P571[天文地球—矿物学]