| 天然状态下岩石密度的μ子测量法 |
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| 引用本文： | 周大庄,马福胜,程纯杰. 天然状态下岩石密度的μ子测量法[J]. 中国科学技术大学学报, 1989, 0(1) |
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| 作者姓名： | 周大庄 马福胜 程纯杰 |
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| 作者单位： | 中国科学技术大学地球与空间科学系(周大庄，马福胜)，中国科学技术大学地球与空间科学系(程纯杰) |
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| 基金项目： | 国家305项目，国家自然科学基金 |
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| 摘 要： | 地下μ子强度随岩石深度的增加减弱。利用地下μ子的强度-深度关系能够测量天然状态岩石密度。此法可测μ子望远镜上方任意方向的岩石平均密度。
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| 关 键 词： | 地下宇宙线 μ子强度 岩石密度 地质应用 |
The Measurement Method of Rock Density in Natural State Through Muon Intensities |
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| Zhou Dazhuang,Ma Fusheng,Cheng Chunjie Dept. of Earth and Space Science. The Measurement Method of Rock Density in Natural State Through Muon Intensities[J]. Journal of University of Science and Technology of China, 1989, 0(1) |
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| Authors: | Zhou Dazhuang Ma Fusheng Cheng Chunjie Dept. of Earth Space Science |
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| Affiliation: | Zhou Dazhuang;Ma Fusheng;Cheng Chunjie Dept. of Earth and Space Science |
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| Abstract: | The intensity of underground cosmic-ray muons decreases when the rockdepth increases. The rock density in natural state can be measured throughintensity-depth relations of underground muons. This method can preciselymeasure the average densities of rocks with any thickness up to the order of1000 meter in any direction above the muon telescopy. |
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| Keywords: | underground cosmic rays muon intensity rock density Applications in geologies |
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