| 论天然水晶形成机制 |
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| 引用本文： | 郑大中,郑若锋.论天然水晶形成机制[J].云南地质,2005,24(1):22-31. |
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| 作者姓名： | 郑大中 郑若锋 |
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| 作者单位： | 成都综合岩矿测试中心,四川,成都,610081 |
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| 摘 要： | 通过对石英、硅酸的物理性质,水晶晶洞、水晶矿床矿物流体包裹成分,不同颜色紫晶的痕量成分,水晶的共生、伴生矿物组合等相关问题的研讨,认为水晶的形成机制为:以硅氢化物气态形式迁移、分异、富集,在稳定、温和、宽松环境被缓慢氧化、水解,自由结晶成单晶和(或)晶簇的。
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| 关 键 词： | 硅氢化物 天然水晶 形成机制 |
| 文章编号： | 1004-1885(2005)01-022-010 |
A NEW RESEARCH OF THE FORMATION MECHANISM OF CRYSTAL |
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| ZHENG Da-zhong,ZHENG Ruo-feng.A NEW RESEARCH OF THE FORMATION MECHANISM OF CRYSTAL[J].Yunnan Geology,2005,24(1):22-31. |
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| Authors: | ZHENG Da-zhong ZHENG Ruo-feng |
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| Abstract: | According to the study on the physical quality of quartz, silica, crystal miarolitic cavity, fluid inclusion composition in mineral of crystal deposit, the trace constituent of amethyst with different color, the paragenesis of crystal, the assemblage of associate mineral, etc, we believe that the formation mechenism of crystal is as follows. The siliceous hydride is migrated in gaseous state, differentiated, enriched, then oxided slowly, hydrolyzed, becomes monocrystal and(or) druse by the free crystallization under a stable, mild and broad environment. |
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| Keywords: | Natural Crysta Siliceous Hydride Formation Mechanism |
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