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西宁市光明小区浅震成果
引用本文:胡玉青.西宁市光明小区浅震成果[J].地球科学与环境学报,1987(3).
作者姓名:胡玉青
作者单位:青海省物探队
摘    要:隐蔽层是初至波方法不能探测到的速度层,它影响着初至波法的解释精度,本文讨论了隐蔽层存在的条件,并提出利用续至波探测隐蔽层的思路

关 键 词:隐蔽层  初至波  续至波

SHALLOW SEISMIC RESULTS IN THE GUANG MIN DISTRICT, XINNING CITY
Hu Yuqing.SHALLOW SEISMIC RESULTS IN THE GUANG MIN DISTRICT, XINNING CITY[J].Journal of Earth Sciences and Environment,1987(3).
Authors:Hu Yuqing
Institution:Geophysical Prospecting Team of Qinghai Province
Abstract:The hidden layer is a velocity one that cannot be detected by the head-wave analysis. It affects the explanation accuracy of the head-wave analysis. This paper deals with the existing conditions of the hidden layer and puts forward the idea to detect it by means of the later-wave.
Keywords:hidden layer  head-wave  later-wave
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