Time frequncy(T-F) analysis is a method studying thin interbedding structure onthe base of T-F changing pattern of seimic response.
析根据震响应的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.
析根据震响应的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.
过渡区岩性以火山碎屑岩沉积岩互层为特征,夹少量火山熔岩;
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