海拉尔盆地火山碎屑岩的成岩作用

程日辉, 沈艳杰, 颜景波, 李庆峰, 李晓辉, 王英武, 李飞, 许中杰. 海拉尔盆地火山碎屑岩的成岩作用[J]. 岩石学报, 2010, 26(1): 47-54.
引用本文: 程日辉, 沈艳杰, 颜景波, 李庆峰, 李晓辉, 王英武, 李飞, 许中杰. 海拉尔盆地火山碎屑岩的成岩作用[J]. 岩石学报, 2010, 26(1): 47-54.
CHENG RiHui, SHEN YanJie, YAN JingBo, LI QingFeng, LI XiaoHui, WANG YingWu, LI Fei, XU ZhongJie. Diagenesis of volcaniclastic rocks in Hailaer Basin[J]. Acta Petrologica Sinica, 2010, 26(1): 47-54.
Citation: CHENG RiHui, SHEN YanJie, YAN JingBo, LI QingFeng, LI XiaoHui, WANG YingWu, LI Fei, XU ZhongJie. Diagenesis of volcaniclastic rocks in Hailaer Basin[J]. Acta Petrologica Sinica, 2010, 26(1): 47-54.

海拉尔盆地火山碎屑岩的成岩作用

  • 基金项目:

    本文受国家“973”项目(2009CB219303)和国家自然科学基金项目(40972074)联合资助.

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Diagenesis of volcaniclastic rocks in Hailaer Basin

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  • 对来自海拉尔盆地40口井的白垩系火山碎屑岩样品显微镜观察与分析显示,火山碎屑岩的成岩作用具有特殊性,表现在熔结作用、脱玻化与重结晶作用、粘土矿物形成与转变和交代作用等方面。熔结作用可以区分出熔浆/熔岩熔结、浆屑熔结和热灰熔结三种类型。脱玻化与重结晶作用常常是交织在一起,流纹质玻璃物质经脱玻化,并进一步重结晶,常具有特殊的结构,呈现一种复杂的硅质胶结样式。粘土矿物形成与转变在成岩作用早期就开始了,如蒙脱石化。一些特征性矿物如浊沸石、绿泥石的出现也不代表变质作用的开始,而是特定成岩环境的产物。碳酸盐的交代-胶结和溶解在火山碎屑岩中普遍发育,使得原岩面貌发生了严重的改变。成岩作用的特征揭示海拉尔盆地火山碎屑岩的成分和结构演变,这在测井岩性解释和孔隙度预测上具有意义。
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出版历程
收稿日期:  2009-07-04
修回日期:  2009-11-10
刊出日期:  2010-01-31

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