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浙江花岗岩的交代作用研究(英文)

Metasomatic Alteration of Granitic Rocks in Zhejiang Province of China

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【作者】 穆罕默德·埃罗密勒巩恩普孙旭东陈兴华

【Author】 Moustafa Elomella, CONGEnpu, SUN Xudong, CHEN Xinghua(Northeastern University, Shenyang 110004, China; Geology Department of Suez Canal University, Ismailia, Egypt)

【机构】 东北大学东北大学 沈阳 110004 Geology Department of Suez Canal UniversityIsmailiaEgypt沈阳 110004沈阳 110004

【摘要】 用岩相学方法研究浙江花岗岩的交代作用。浙江花岗岩的主要交代过程包括交代引起的碱性化,如绢云母化、微斜长石化和硅化。斜长石的绢云母化大量发生在低温低压条件区域,随热液进入,带入了过量水、K、Al和Si。在交代作用后期,更多的花岗岩形成,这些花岗岩可再熔化,熔化后又会凝固并被交代流体作用。

【Abstract】 Metasomatism of the granitic rocks in Zhejiang Province, China is investigated by petrography. The meta-somatic processes predominating in the granitic rocks in Zhejiang Province include alkali enrichment caused by metasomatism, i.e. seriatization, microclirization, and silicification. Sericitization of plagioclase occurs on a large scale in the area at low temperature-pressure conditions, and additional water, K, Al, and Si are brought in as a result of hydrothermal fluids entering. More granitic rocks are produced in the late-stage of metasomatism, which could be remelt, and each successive melt could be solidified and modified by metasomatic fluids.

【基金】 National Nature Science Foundation of China (40072006);The Key Task Project of Science and Technology of Liaoning Province (2001230001) 国家自然科学基金(40072006);辽宁省“十五”科技攻关项目(2001230001)
  • 【分类号】P588.1
  • 【下载频次】56
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