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资阳地区震旦系灯影组白云岩中葡萄花边的成因研究

STUDYING ON THE ORIGIN OF BOTRYOIDAL LACE IN DOLOMITITE OF DENGYING FORMATION, SINIAN FROM ZIYANG SICHUAN

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【作者】 向芳陈洪德张锦泉

【Author】 Xiang Fang Chen Hongde Zhang Jinquan (Institute of Sedimentary Geology,Chengdu University of Technology , Chengdu 610059)

【机构】 成都理工学院沉积地质研究所

【摘要】 资阳地区灯影组为一套形成于潮坪环境、以藻白云岩为主的地层,岩层中发育大量的葡萄花边构造。通过对葡萄花边、藻白云岩、充填白云石进行岩矿鉴定、电镜扫描、X射线衍射、碳氧同位素、微量元素等的分析,并结合本区成岩演化史,认为葡萄花边有两种成因:(1)准同生混合水成因;(2)表生混合水成因。葡萄花边的存在,能够指示溶蚀作用的存在,因而对研究古岩溶储层具有重要意义。

【Abstract】 Dengying Formation of Sinian is a set of algal dolomitite forming at tidal flat, and in which the botryoidal lace can be often seen. Throng studying in very detailed by a series analysis such as: thin section, SMZ, X ray diffraction, isotopes, traces elements of botryoidal lace, protolith and filling dolomites, it can be disclosed that botryoidal lace has two kinds of origins: a. penecontemporaneous mixing water origin; b. epigenetic mixing water origin. Because the botryoidal lace can indicate dissolution(especially palo karst), it has the important significance for the study of palo karst reservoirs.

  • 【文献出处】 矿物岩石 ,JOURNAL OF MINERALOGY AND PETROLOGY , 编辑部邮箱 ,1998年S1期
  • 【分类号】P588.245
  • 【被引频次】46
  • 【下载频次】501
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