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黑云母与氯化物热水溶液相互作用的实验研究

ERACTION BETWEEN BIOTITE AND CHLORIDE HYDROTHERM FLUID──AN EXPERIMENTAL STUDY

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【作者】 曾贻善冯钟燕郝吉成

【Author】 Zeng Yishan; Feng Zhongyan; Hao Jicheng (Department of Geology. Peking University, Beijing, 100871)

【机构】 北京大学地质系!北京100871

【摘要】 本文在500℃和1×108Pa条件下,利用冷封口高温高压水热系统和焊封金管技术实验研究了黑云母和Na-Ca-氯化物溶液的相互作用,着重考察反应不同时间的黑云母表面和溶液化学的变化。黑云母中的K、Fe和Si不同程度地进入溶液相,而溶液中原有的Na和Ca含量降低;SEM/EDAX和EMAX研究表明,反应后的黑云母边缘部分明显失去K和Fe,应得到相当数量的H2O和一些Ca。黑云母中Fe活化的控制反应可能是H+交代作用。

【Abstract】 Using a standard cold-sealed high pressure and high temperature hydrothermal system and sealed gold capsule techniques,changes in solution chemistry and biotite surface after reaction with Na-Ca-chloride solutions for different times at 500℃ and 1 ×108Pa were experimentally studied.K,Fe and Si in biotite were transported into the fluid phase and the Na and Ca contents in the starting solution decreased to a certain extcnt. SEM/EDAX and EMAX studies indicated that at the marginal part of biotite K and Fe were eridently lost,and a considerable amoUnt of H2O and some Ca were gained. The reaction controlling hydrothermal alteration of biotite and Fe mobilization in the mineral is probably H+-metasomatism.

【基金】 国家自然科学基金;北京大学分析测试基金
  • 【文献出处】 矿物学报 ,Acta Mineralogica Sinica , 编辑部邮箱 ,1995年01期
  • 【分类号】P571
  • 【被引频次】1
  • 【下载频次】57
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