| 佛子岭群的岩石地球化学及构造环境 |
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| 引用本文： | 刘贻灿，徐树桐，江来利，苏文.佛子岭群的岩石地球化学及构造环境[J].安徽地质,1996(2). |
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| 作者姓名： | 刘贻灿，徐树桐，江来利，苏文 |
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| 作者单位： | 安徽省地质科学研究所 |
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| 摘 要： | 大别山北部佛子岭群变碎屑岩主要由板岩、千枚岩和云母石英片岩等所组成。其原岩主要为杂砂岩和岩屑砂岩，少数为长石砂岩等。佛子岭群的岩石地球化学及岩石建造特征等均表明，它形成于中朝大陆板块南部活动大陆边缘环境，是一套复理石建造。
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| 关 键 词： | 佛子岭群，岩石地球化学构造，环境，大别山 |
THE PETROGEOCHEMISTRY AND TECTONIC SETTING OF THE FOZILING GROUP |
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| Liu Yican; Xu Shutang; Jiang Laili; Su Wen.THE PETROGEOCHEMISTRY AND TECTONIC SETTING OF THE FOZILING GROUP[J].Geology of Anhui,1996(2). |
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| Authors: | Liu Yican; Xu Shutang; Jiang Laili; Su Wen |
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| Abstract: | Foziling Group in the Dabie Mountains is composed of slate,phyllite,mica quartz schist,etc.Their primary rocks were mainly graywacke, debris sandstone and few feldspar sandstone, ext. The petrologic geochemical characteristics of Fozliling Group indicate that it formed in the active continental margin in south area of Sino Korea continental Plate and is a flysch formation. |
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| Keywords: | Foziling Group Petrogeochemistry tectonic setting Dabie Mt s |
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