夏宇靖. 稳态瑞雷波实测洞穴D-vR曲线的类型[J]. 煤田地质与勘探, 1996, 24(1): 50-55.
引用本文: 夏宇靖. 稳态瑞雷波实测洞穴D-vR曲线的类型[J]. 煤田地质与勘探, 1996, 24(1): 50-55.
Xia YuJing. TYPES OF D-vR CURVE OF CAVERN MEASURED BY STEADY-STATE RAYLEIGH WAVE[J]. COAL GEOLOGY & EXPLORATION, 1996, 24(1): 50-55.
Citation: Xia YuJing. TYPES OF D-vR CURVE OF CAVERN MEASURED BY STEADY-STATE RAYLEIGH WAVE[J]. COAL GEOLOGY & EXPLORATION, 1996, 24(1): 50-55.

稳态瑞雷波实测洞穴D-vR曲线的类型

TYPES OF D-vR CURVE OF CAVERN MEASURED BY STEADY-STATE RAYLEIGH WAVE

  • 摘要: 瑞雷波勘探对洞穴、硫松带等地质体的判断主要根据D-vR曲线形态变化表现的异常特征进行,这在很大程度上有赖于解释者的实践经脸。作者根据多年的实践,把洞穴类地质体表现的异常特征归纳为类,分别举例加以说明,为瑞雷波方法的推广应用及进一步实现解释工作的程序化、自动化,提供了必要的基础资料。

     

    Abstract: Abstract In Rayleigh wave prospecting,the diagnosis of geologic bodies,such as cavern, weaker zone and so on,are still based primarily on the abnormal features which are expressed by the variations of D-vR curve morphology,and they are depended largely on the practical experience of interpreter. Based on many year's practices, the abnormal features expressed by the geologic bodies like cavern are divided into 6 kinds by the author, and illustrated with examples. Therefore,it provides the foundational data for spreading the application of Rayleigh wave method and futher realizing the programmed control and automatization of interpretation.

     

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