前面是陡深的V字形峡谷,水流倾泻而下。
提出了在山高、坡陡、地下水位埋深较大的山丘地区找水,应以寻找低值异常为主的观点,并分析了形成低值异常的基本原因。
According to the low value abnormality we have put forward the method of finding water in places of mountains, steep slope and hill where water table level is embebed deeply.
所提方法扩大了可测深度范围,可用于测量面形较陡的连续表面或不连续深结构表面。
Advantage of the approach is that the depth measurement range is expanded very much, it can be used to measure the profile of the deep or discontinuous surface.
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