Time frequncy(T-F) analysis is a method studying thin interbedding structure onthe base of T-F changing pattern of seimic response.
时频分析根据震响应的时频变化规律研究薄互层结构的一种方法。
Time frequncy(T-F) analysis is a method studying thin interbedding structure onthe base of T-F changing pattern of seimic response.
时频分析根据震响应的时频变化规律研究薄互层结构的一种方法。
The transitional zone is characterized by interbedding of pyroclastic and sedimentary rocks,and a little volcanic lava rocks was also found in the strata.
过
性以火山碎屑
沉积互层为特
，
量火山熔；
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