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红层中水-岩作用微观信息特征及对孔隙演化的影响--以兖州矿区为例
引用本文:吴恩江,韩宝平,王桂梁.红层中水-岩作用微观信息特征及对孔隙演化的影响--以兖州矿区为例[J].中国矿业大学学报,2005,34(1):123-128.
作者姓名:吴恩江  韩宝平  王桂梁
作者单位:1. 中国科学技术大学,地球与空间科学学院,安徽,合肥,230026
2. 中国矿业大学,环境与测绘学院,江苏,徐州,221008
摘    要:利用高分辨实验观察,对取自兖州矿区的251块岩样进行了系统分析,直观地揭示了红层孔隙中多种矿物相及其组合特征,并探讨了其成因.结合岩样的微孔结构测试成果,指出红层孔隙中的水一岩作用过程就是其孔隙空间的再分配过程,并建立了红层中水一岩作用影响下孔隙结构的演化模式.所获结果对于深化认识红层孔隙形态、精确划分富水层段位置等具有重要指导作用.

关 键 词:红层  孔隙演化  水-岩作用  岩样  矿物  演化模式  组合特征  兖州矿区  成果
文章编号:1000-1964(2005)01-0123-06
修稿时间:2004年5月11日

Micro-Information of Water-Rock Interaction and Its Influence on Pore Evolution of Red-Bed in Yanzhou Mining Area
WU En-jiang,HAN Bao-ping,WANG Gui-liang.Micro-Information of Water-Rock Interaction and Its Influence on Pore Evolution of Red-Bed in Yanzhou Mining Area[J].Journal of China University of Mining & Technology,2005,34(1):123-128.
Authors:WU En-jiang  HAN Bao-ping  WANG Gui-liang
Affiliation:WU En-jiang~1,HAN Bao-ping~2,WANG Gui-liang~2
Abstract:According to the results of high resolution experimental observation for 251 rock samples from Yanzhou mining area, various mineral phases and assemblages in pores of red-bed are revealed and their genesis discussed. Based on the analysis of micro-structure test of rock samples, the authors hold that the course of water-rock interaction (WRI) in red-bed is the re-distribution process of its pore space and have established the structure mode of pores evolved under the influence of water-rock interaction. The results are helpful for further understanding of pore forms and for accurately dividing the rich water-bearing layers in red-bed.
Keywords:water-rock interaction  micro-information features  pore evolution  Yanzhou mining area
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