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机构地区:[1]成都理工大学工程技术学院,四川乐山614007 [2]东华理工学院,江西抚州344000
出 处:《铀矿地质》2008年第5期298-301,共4页Uranium Geology
摘 要:本文将土壤天然热释光方法应用于寻找滑坡体边界,发现推测边界与实际边界相近,表明该方法探查滑坡体边界效果明显,有良好的应用前景。Soil natural thermoluminescence survey is a accumulation measuring method which can measure radon for long time. Its sensitivity and repeatability are much better than other usual methods, so it has been widely used in the geological field. In the paper, the method is used to prospect the boundary of slide body. The inferred boundary was found near the real boundary, the survey indicates that the measurement result is outstanding and this method has good application vista.
分 类 号:P631.622[天文地球—地质矿产勘探]
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