地震地质 ›› 1993, Vol. 15 ›› Issue (3): 277-284.

• 科研简报 • 上一篇    下一篇

GRM法对江苏HQ—13线Pg波折射资料的再解释

章惠芳, 谢剑波   

  1. 广东省地震局, 广州 510070
  • 收稿日期:1990-10-31 修回日期:1993-02-28 出版日期:1993-09-01 发布日期:2009-11-25
  • 基金资助:
    地震科学联合基金资助(88394)

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

Zhang Huifang, Xie Jianbo   

  1. Seismological Bureau of Guangdong Province, Guangzhou 510070
  • Received:1990-10-31 Revised:1993-02-28 Online:1993-09-01 Published:2009-11-25

摘要: 用一种新的折射解释法——广义互换法(GRM),对江苏HQ-13线Pg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ToTp法更精确。

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

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 ToTp method.

Key words: Velocity analysis function, Time-depth relation, Refraction layer velocity, Depth-conversion factor, Optimum XY value, Jiangsu, General reciprocal method