The seismic channel P waves phi-g or P and their propagation along the crust of the Indian sub-continent

Most read articles by the same author(s)

• B. P. SAHA, ON THE DEPTH OF FOCUS OF THE DELHI EARTHQUAKE OF 27 AUGUST 1960 , MAUSAM: Vol. 13 No. 1 (1962): MAUSAM
• B. P. SAHA, PcA OR ScP PHASE AND THE DEPTH OF EARTHQUAKE FOCUS , MAUSAM: Vol. 13 No. 3 (1962): MAUSAM
• B. P. SAHA, A seismometric study of the Russian Nuclear Explosion on 30 October 1961 , MAUSAM: Vol. 13 No. 2 (1962): MAUSAM
• B. P. SAHA, The seismic Lg waves and their propagation along the granitic layer of the crust of Indian Sub-Continent , MAUSAM: Vol. 12 No. 4 (1961): MAUSAM
• B. P. SAHA, An account of short period microseisms recorded during three Indian cyclones , MAUSAM: Vol. 15 No. 3 (1964): MAUSAM
• B. P. SAHA, Determination of Sedimentary Thickness in the Shillong plateau by Microseisms , MAUSAM: Vol. 13 No. 2 (1962): MAUSAM
• B. P. SAHA, M2 or first shear mode continental Rayleigh waves from Russian nuclear explosion of 30 October 1961 , MAUSAM: Vol. 16 No. 2 (1965): MAUSAM
• B. P. SAHA, R. MOHAN, A note on the sense of the first PKP motion for the Peru-Brazil border earthquake of 19 August 1961 , MAUSAM: Vol. 14 No. 2 (1963): MAUSAM
• B. P. SAHA, Structure of Microseisms from Bay of Bengal , MAUSAM: Vol. 17 No. 3 (1966): MAUSAM
• B. P. SAHA, Distribution of energy in p and S Seismic bodily waves , MAUSAM: Vol. 17 No. 3 (1966): MAUSAM