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江西大吉山五里亭花岗岩中变生褐帘石的加热研究
引用本文:陶克捷.江西大吉山五里亭花岗岩中变生褐帘石的加热研究[J].地质科学,1992,0(4):399-403.
作者姓名:陶克捷
作者单位:中国科学院地质研究所, 北京 100029
摘    要:对采自我国南方燕山期五里亭花岗岩体中的褐帘石,经偏光显徽镜、电子探针仪、差热仪、X射线等方法进行分析得出,该矿物为变生褐帘石。加热800℃,850℃,950℃,970℃,1100℃退火系列样品的X射线粉晶数据分析得出:1.变生褐帘石X射线粉晶分析的最宜加热温度为800-850℃;2.加热至970℃的退火样品,褐帘石已分解为方铈石、赤铁矿、钙长石,加热到1100℃,褐帘石已渐消失,方铈石、钙长石和赤铁矿成为主要矿物相。

关 键 词:变生褐帘石  退火样品的X射线衍射分析  方铈石  赤铁矿  钙长石
收稿时间:1990-12-01
修稿时间:1990-12-01;

A STUDY ON HEAT TREATMENT OF METAMICT ALLANITE IN SOUTH CHINA
Tao Kejie.A STUDY ON HEAT TREATMENT OF METAMICT ALLANITE IN SOUTH CHINA[J].Chinese Journal of Geology,1992,0(4):399-403.
Authors:Tao Kejie
Institution:Institute of Geology, Academia Sinica, Beijing
Abstract:The metamict allanite from South China is studied by using microscopy, DTA and X-ray powder analyses. The results show that the annealed sample heated to 800 ——850(3 gives the standard X-ray data of allanite, and the sample heated over 850℃ is decomposed. The annealed sample heated to 970℃ is decomposed into cerianite, hematite, anorthite and small amount of allanite and other minerals. From the X-ray powder data the reaction process may be expressed as: 2(Ca, Ce)(Fe). X-ray powder data of the anneaied allanite heated to 11000(2 show that the allanite was decomposed into dominant cerianite, hematite, and anorthite, but allanite disappeared.
Keywords:granite  metamict allanite  X-ray powder analysis  cerianite  hematite  anorthite
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