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- W2389092227 abstract "The records obtained from the low-frequency refraction work carried out in Chaitamu Basin are characterized by multiple waves. It is found that within two or three kilometres from the earth's surface, there exist several zones which possess velocity gradien. Seismic rays are refracted back to the earth's surface when they graze these zones of varying velocities. These refracted waves have undergone little energy conversion; therefore their high order multiples can be detected with appreci- able intensities even at a distance of 10-30 kilometres from the shot point. The multiples obtained in Chaitamu Basin consist of the following: (i) curved rays multiply reflected at the earth's surface, (ii) reflection-head waves, (iii) head wave-reflections, and (iv) mul- tiple reflections. The properties of these multiple waves and the methods of their discriminations are described. It is noticed that there is some directional effect in receiving these multiple waves, and the cause for this is discussed." @default.
- W2389092227 created "2016-06-24" @default.
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- W2389092227 date "1962-01-01" @default.
- W2389092227 modified "2023-09-26" @default.
- W2389092227 title "REFRACTED WAVES AND MULTIPLE WAVES IN CHAITAMU BASIN BY LOW-FREQUENCY SEISMIC REFRACTION METHOD" @default.
- W2389092227 hasPublicationYear "1962" @default.
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