华南花岗岩残积土红土化程度的地带性与香港该类土不发育的原因

曲永新 吴宏伟 尚彦军

曲永新, 吴宏伟, 尚彦军. 2000: 华南花岗岩残积土红土化程度的地带性与香港该类土不发育的原因. 工程地质学报, 8(1): 16-20.
引用本文: 曲永新, 吴宏伟, 尚彦军. 2000: 华南花岗岩残积土红土化程度的地带性与香港该类土不发育的原因. 工程地质学报, 8(1): 16-20.
QU Yong xin, Ng Wang Wai Charles, SHANG Yan jun. 2000: STUDY ON LATITUDINAL EFFECT ON LATERITIZATION OF ELUVIAL SOIL ON GRANITE AND CUASE FOR WEAK LATERITIZATION OF THE SOIL IN HONGKONG. JOURNAL OF ENGINEERING GEOLOGY, 8(1): 16-20.
Citation: QU Yong xin, Ng Wang Wai Charles, SHANG Yan jun. 2000: STUDY ON LATITUDINAL EFFECT ON LATERITIZATION OF ELUVIAL SOIL ON GRANITE AND CUASE FOR WEAK LATERITIZATION OF THE SOIL IN HONGKONG. JOURNAL OF ENGINEERING GEOLOGY, 8(1): 16-20.

华南花岗岩残积土红土化程度的地带性与香港该类土不发育的原因

详细信息
    作者简介:

    曲永新(1937-),男,教授,工程地质专业.

  • 中图分类号: P642.132

STUDY ON LATITUDINAL EFFECT ON LATERITIZATION OF ELUVIAL SOIL ON GRANITE AND CUASE FOR WEAK LATERITIZATION OF THE SOIL IN HONGKONG

  • 摘要: 从华南花岗岩残积土红土化程度的地域变化规律出发 ,通过香港与华南沿海各地花岗岩残积土的化学成分及红土化指标对比 ,作者发现香港花岗岩残积土无论厚度、类型 ,还是红土化程度都具有与所处气候环境不协调的特点。文章进一步讨论了香港花岗岩残积土不发育的原因和对工程性质的影响.
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出版历程
  • 收稿日期:  1998-10-10
  • 修回日期:  1999-01-20
  • 刊出日期:  2000-01-22

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