陈跃志, 桑宝梁. 1995: 佛子岭群变质岩石学变质作用及时代的初步研究. 地质通报, (3).
    引用本文: 陈跃志, 桑宝梁. 1995: 佛子岭群变质岩石学变质作用及时代的初步研究. 地质通报, (3).
    1995: METAMORPHIC PETROLOGY AND METAMORPHISM OF THE FOZILING GROUP IN NOTHERN HUAIYANG AND ITS AGE. Geological Bulletin of China, (3).
    Citation: 1995: METAMORPHIC PETROLOGY AND METAMORPHISM OF THE FOZILING GROUP IN NOTHERN HUAIYANG AND ITS AGE. Geological Bulletin of China, (3).

    佛子岭群变质岩石学变质作用及时代的初步研究

    METAMORPHIC PETROLOGY AND METAMORPHISM OF THE FOZILING GROUP IN NOTHERN HUAIYANG AND ITS AGE

    • 摘要: 佛子岭群是北淮阳地区分布较广的地层单位之一。主要岩石类型为长石石英岩、细粒石英岩、含蓝晶石英片岩和含石英白云质大理岩。变质矿物有蓝晶石、石格石、黑云母及白云母等。根据石榴石一黑云母矿物对计算温度约520℃,压力为0.3~0.5GPak。主变质作用年龄为378±24Ma。

       

      Abstract: The Foziling Group is one of the widespread stratigraphic units in northern Huaiyang,Themain rock types of the group are arkosite,fine-grained quartzite,glaucophane-bearing quartzschist,and quartz-bearing dolomitic marble. The metamorphic age of the group is 378±24 Ma.The metamorphic minerals include glaucophane,garnet, biotite and muscovite. The metamor-phic temperature calculated with the garnet-biotite mineral pair is about 520℃ and the pressureis 0.3 0.5 GPa.

       

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