侵入岩的镁铁云母化学成分特征及其地质意义
CHEMICAL CHARACTERISTICS OF MAFIC MICA IN INTRUSIVE ROCKS AND ITS GEOLOGICAL MEANING
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摘要: 研究镁铁云母对了解原生侵入岩的地质环境有重要意义。本文拟通过原生镁铁云母化学成分及其指数图解,讨论原生岩石的地质环境。研究结果表明,镁铁云母化学成分变化受其物质来源影响,其矿物化学与成矿作用有密切联系。Abstract: A lot of articles on mineral texture, classification and mineralization of mafic mica series bad been published during recent a few years. This paper discusses the indicative geological meaning of material source of the mafic mica series. 35 field samples were collected. At the same time the auther has also synthesized 77 samples from chinese and foreign references. On the basis of research on gto chemistry of some trace elements and REE in marie mica, fellowing conelutions are primarily obtained:1. Change of chemical composition in marie mica was contraled obviously by the material source environment.2. Chemical composition of the mafic mica is closely related with mineralization.3. The change in (Fe~(+3)+Fe~(+2))-Mg content in mineral composition has been closer relation to the geological emironment and mineralization.4. The variation in chemical composition of svitalshite has certain indicative meaning for the material source of intrusive rocks.
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Key words:
- Svitalskite /
- Granite of crust type /
- Granite of mantle-crust migmatite type /
- Mantle
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