论文部分内容阅读
根据在大城地区用数字仪进行的地震方法试验,说明在方法合理、地震地质条件合适的情况下,使用地震方法了解古生界(主要是下古生界)侵蚀面及其内幕结构是可能的。文章展示和解释了实际资料。
According to the seismic method test carried out by the digital instrument in Ayutthaya, it is possible to use the seismic method to understand the erosion surface of the Paleozoic (mainly the Lower Paleozoic) and its internal structure when the method is reasonable and the seismic geological conditions are appropriate . The article shows and explains the actual data.