| GRM 法对江苏 HQ-13线 P_g 波折射资料的再解释 |
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| 引用本文： | 章惠芳 谢剑波. GRM 法对江苏 HQ-13线 P_g 波折射资料的再解释[J]. 地震地质, 1993, 15(3): 277-284 |
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| 作者姓名： | 章惠芳 谢剑波 |
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| 作者单位： | 广东省地震局，广东省地震局 广州 510070，广州 510070 |
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| 摘 要： | 用一种新的折射解释法——广义互换法(GRM),对江苏HQ-13线P_g波资料进行了解释。GRM法打破了传统的解释程序,先用计算机处理,后解释,其结果既客观又省时,不但能显著提高经济效益,而且经钻井资料证明它的解比T_oT_p法更精确
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| 关 键 词： | 速度分析函数 时-深函数 折射层速度 深度转换因子 最佳XY值 江苏 广义 互换法 |
REINTERPRETATION OF Pg WAVE REFRACTION DATA ALONG PROFILE HQ-13 IN JIANGSU BY GRM METHOD |
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| Zhang Huifang Xie Jianbo. REINTERPRETATION OF Pg WAVE REFRACTION DATA ALONG PROFILE HQ-13 IN JIANGSU BY GRM METHOD[J]. Seismology and Geology, 1993, 15(3): 277-284 |
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| Authors: | Zhang Huifang Xie Jianbo |
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| Abstract: | In this paper, a new method, general reciprocal method(GRM), is used in interpretation of Pg wave data along HQ-13 line in Jiangsu Province. By the GRM method, wave data are firstly processed on microcomputer and then interpreted. The procedure is more fast and more effective than traditional method. The result of processing of drill data comfirms that the GRM solution is more accurate than that of T0Tpmethod. |
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| Keywords: | Velocity analysis function Time-depth relation Refraction layer velocity Depth-conversion factor Optimum XY value Jiangsu General reciprocal method |
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