THE DISTURBANCE DUE TO A LINE SOURCE IN A SEMI-INFINITE ELASTIC MEDIUM

[1] Bromwich T. J. J. A., 1898, P LOND MATH SOC, V30, P98, DOI [10.1112/plms/s1-30.1.98, DOI 10.1112/PLMS/S1-30.1.98]

[2] BYERLY P, 1940, T AM GEOPH U, V4, P1117

[3] Fu CY., 1947, GEOPHYSICS, V12, P57, DOI [10.1190/1.1437297, DOI 10.1190/1.1437297]

[4] Jahnke E, 1945, TABLES FUNCTIONS

[5] JEFFREYS H, 1946, METHODS MATH PHYSICS

[6] JEFFREYS H, 1931, BEITR GEOPHYS, V30, P336

[7] JEFFREYS H, 1926, MONTHLY NOTICES RO S, V1, P321

[8] JEFFREYS H, 1926, P CAMB PHILOS SOC, V23, P472

[9] Jeffreys H., 1929, EARTH, V4th ed.

[10] JEFFREYS H, 1946, REP PROGR PHYS, V10, P52

[1] Bromwich T. J. J. A., 1898, P LOND MATH SOC, V30, P98, DOI [10.1112/plms/s1-30.1.98, DOI 10.1112/PLMS/S1-30.1.98]

[2] BYERLY P, 1940, T AM GEOPH U, V4, P1117

[3] Fu CY., 1947, GEOPHYSICS, V12, P57, DOI [10.1190/1.1437297, DOI 10.1190/1.1437297]

[4] Jahnke E, 1945, TABLES FUNCTIONS

[5] JEFFREYS H, 1946, METHODS MATH PHYSICS

[6] JEFFREYS H, 1931, BEITR GEOPHYS, V30, P336

[7] JEFFREYS H, 1926, MONTHLY NOTICES RO S, V1, P321

[8] JEFFREYS H, 1926, P CAMB PHILOS SOC, V23, P472

[9] Jeffreys H., 1929, EARTH, V4th ed.

[10] JEFFREYS H, 1946, REP PROGR PHYS, V10, P52