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新疆富钕褐帘石的首次发现及矿物学特征
引用本文:丁奎首 张培善. 新疆富钕褐帘石的首次发现及矿物学特征[J]. 地质科学, 1994, 29(1): 93-95
作者姓名:丁奎首 张培善
作者单位:中国科学院地质研究所 北京 100029
摘    要:普通褐帘石多含饰,常呈副矿物存在于花岗岩、矽卡岩、火山灰(Izett,1981、变质泥岩(Sakai er al., 1984)等岩类.本文所报道的近年发现的一种富教褐帘石,产于新疆哈图金矿外围伟晶石英脉中.该矿物深黑色,呈单斜柱状晶簇,晶体最长可达10cm以上。

关 键 词:富钕褐帘石  穆斯堡尔谱  变生作用
收稿时间:1992-12-01
修稿时间:1992-12-01;

FIRST DISCOVERY OF Nd-RICH ALLANITE IN XINJIANG AND ITS CHARACTERISTICS
Ding Kuishou,Zhang Peishang,Li Zhe. FIRST DISCOVERY OF Nd-RICH ALLANITE IN XINJIANG AND ITS CHARACTERISTICS[J]. Chinese Journal of Geology, 1994, 29(1): 93-95
Authors:Ding Kuishou  Zhang Peishang  Li Zhe
Affiliation:Institute of Geology Academic Sinica.Beijing 100029
Abstract:The crystal clusters of Nd-rich allanite were first found in Xinjiang by the authors. The mineral is rich in neodymium and without ferric iron.Its structure and physical properties are not different from normal metamict allanite,but there is an obvious difference in their behaviour of iron crystallochemistry.The mineral in this study was thermally decomposed and became a mixture of complicated oxides at temperature above 930℃.
Keywords:Nd-rich allanite  Mossbauer spectrum  Metamictization  
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