GRM 法对江苏 HQ—13线 P_g 波折射资料的再解释  

REINTERPRETATION OF Pg WAVE REFRACTION DATA ALONG PROFILE HQ-13 IN JIANGSU BY GRM METHOD

作　　者：章惠芳[1] 谢剑波[1] 

机构地区：[1]广东省地震局,广州510070

出　　处：《地震地质》1993年第3期277-284,共8页Seismology and Geology

基　　金：地震科学联合基金资助(88394)

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。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.

关 键 词：广义互换法 地震折射波法 GRM法 

分 类 号：P315.63[天文地球—地震学]