| 香花岭地区花岗岩类岩石稀土元素演化特点及其形成机理的探讨 |
| 点此下载全文 |
| 引用本文：杜绍华,邱瑞照.1989.香花岭地区花岗岩类岩石稀土元素演化特点及其形成机理的探讨[J].地球学报,11(1):131-142. |
| DOI： |
| 摘要点击次数: 4117 |
| 全文下载次数: 4801 |
|
|
| 中文摘要:随着岩浆的演化,香花岭地区花岗岩类岩石的稀土元素总量不断下降,负铕异常减小,轻稀土相对于重稀土越来越富集,显示了与绝大多数花岗岩类岩石相反的逆向演化特点。造成本区花岗岩类稀土元素逆向演化的原因,除与本区花岗岩浆体系不同演化阶段的氧化还原条件不同外,最根本的是与该岩浆体系向贫Si、(K+Na),富Al、Li、F和H_2O的方向演化所造成的岩浆体系碱度的不断增强有关。 |
| |
| A PRELIMINARY STUDY ON THE REE EVOLUTION CHARACTERISTICS AND THEIR FORMATION MECHANISM OF THE GRANITOIDS IN XIANGHUALING (HSIANGHUALING) DISTRICT |
|
|
| Abstract:In the Xianghualing (Hsianghualing) district, South Hunan, there are mainly three types of granitoids, i. e, the biotitegranite, zinnwaldite-albite-granite and Hsianghuagite. These granitoid rocks are formed by the same granitic magma in different stages and constitute a complete magmatic evolutionary series.With the magma evolving, the REE contents and negative Eu anomaly decrease progressively, and the LREE are more and more enriched as compared with HREE. Abovementioned facts show an evolutionary tendency of REE of the granitoids in the study district contrary to that of the granitoids elsewhere.The components of the granitic magma system become poorer in Si,(K + Na), richer in Al, Li, F and H2O+ during the evolution, which caused weaker acidity and stronger alkalinity. It may be the most important reason for the specific REE evolution of the granitoids in this district. In addition, the varied oxidation-reduction environments in different evolutionary stages of this magmatie system may be the other reason. |
| 查看全文 查看/发表评论 下载PDF阅读器 |
|
|
|
|
|
