佛子岭镇
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REE和微量元素特征显示肥西地区中生代砂岩物源主要为佛子岭群和卢镇关群,大别杂岩的影响比较局限,更没有来自华北克拉通的物质。
The data of REE and trace elements indicate that the source rocks were mainly composed of Fuziling and Luzhengguan Groups , limited for Dabie complex and no Huabei Landmass matter .
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大别山北部的变质复理石推覆体属华北大陆板块南部的盖层推覆体,主要包括佛子岭群和卢镇关群。
The meta flysch nappe in the north part of the Dabie Mountains is composed of the Foziling Group and Luzhenguan Group .