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- W2381774575 abstract "The methods of studying the hthospheric structure with seismic wave field mainly include natural source teleseismic observation,near seismic observation and artificial source deep seismic profiling.The source of artificial deep seismic profiling is located in the surface medium,and source location,detonation time,receiving condition is precisely known.So the result from deep seismic profiling is the most accurate.Artificial source deep seismic profiling is divided into two parts.One is deep seismic sounding;the other is deep seismic reflection.From the first part,we can get crust and upper mantle structure and velocity distribution,and from the other part,we can know the detailed crust structure.These two methods have their own characteristic and are complementary.Currently,the joint detection of the deep seismic sounding and deep seismic reflection can obtain velocity structure and formation distribution,which must become the necessary method of Hthospheric study." @default.
- W2381774575 created "2016-06-24" @default.
- W2381774575 creator A5051203800 @default.
- W2381774575 date "2014-01-01" @default.
- W2381774575 modified "2023-09-24" @default.
- W2381774575 title "Detection of crust and mantle structures and distinguish of the anomaly body with artificial source deep seismic profiling" @default.
- W2381774575 hasPublicationYear "2014" @default.
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