期刊文献+

峨眉山玄武岩岩体风化分带量化研究 被引量:6

Quantitative Study on the Zoning of Weathering Degree of Emei Mountain Basalts
原文传递
导出
摘要 通过对玄武岩的表观特征、矿物特征、化学特征的研究,发现峨眉山玄武岩的风化作用以物理风化为主,化学风化不明显;运用岩体波速比、岩体的完整性系数、岩石质量指标分别对岩体风化进行了分带;在对岩体分带量化指标研究的基础上,综合确定了峨眉山玄武岩岩体风化分带的量化标准;并以某水电工程边坡为例,运用该标准划分了岩体风化带,总结了斜坡岩体的风化规律.图9,表2,参7. Based on the study of the apparent feature, mineral feature and chemical feature of basalts, the result indicates that the physical weathering of Emei mountain basalts is principal and chemical ,weathering is not obvious. The weathering of rock are zoned in terms of the ratio of wave speed, integrality index of rock mass and rock quality index. Based on quantitative parameters study on the Zoning of rock, the author synthetically determines quantitative standards of belt of weathering. Finally, the slope of a hydropower project as an example, using the standards for dividing the weathered band of rock and summing up the law of weathered rock of slopes.
出处 《湖南科技大学学报(自然科学版)》 CAS 北大核心 2008年第3期32-36,共5页 Journal of Hunan University of Science And Technology:Natural Science Edition
基金 “十一五”国家科技支撑计划资助项目(2006BAJ27B05 2006BAJ05A02)
关键词 峨眉山玄武岩 岩体风化分带 玄武岩的微观结构 波速比 Emei mountain basalt the zoning of weathering degree of rock microstructure of basalts ratio of wave speed
  • 相关文献

参考文献4

  • 1[1]DEERE D U.Technical Description of Rock Cores for Engineering Purposes[J].Rock Mech Eng Geol,1963,1:18-22.
  • 2[2]DEERE D U.Gedagieal considerations[C]//StaggKG,ZienkiewicaOC.Rock Mechanics in Engineering Practice.London:Wiley.1968,1-20.
  • 3[3]MERRITT A H.Engineering Chassificatio for in Situ Rock[D].Urbana:Univ lllinois,1968.
  • 4[4]PATtON F D,DEERE D U.Geological Factors Controlling Slope Stability in Open Pit Mines Proc let Int Corf Stability in Open Pit Mining[D].Canada:Vancouver,1970.

同被引文献47

引证文献6

二级引证文献120

相关作者

内容加载中请稍等...

相关机构

内容加载中请稍等...

相关主题

内容加载中请稍等...

浏览历史

内容加载中请稍等...
;
使用帮助 返回顶部