THE DISTURBANCE DUE TO A LINE SOURCE IN A SEMI-INFINITE ELASTIC MEDIUM WITH A SINGLE SURFACE LAYER

[1] Birch F, 1935, BULL GEOL SOC AM, V46, P1219

[2] 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]

[3] BROMWICH TJI, 1916, P LOND MATH SOC, V15, P425

[4] JEFFREYS H, 1926, MON NOT R ASTR SOC S, V1, P282

[5] JEFFREYS H, 1946, METHODS MATH PHYSICS

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

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

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

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

[10] JEFFREYS H, 1935, MON NOT R ASTR SOC S, V3, P257

[1] Birch F, 1935, BULL GEOL SOC AM, V46, P1219

[2] 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]

[3] BROMWICH TJI, 1916, P LOND MATH SOC, V15, P425

[4] JEFFREYS H, 1926, MON NOT R ASTR SOC S, V1, P282

[5] JEFFREYS H, 1946, METHODS MATH PHYSICS

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

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

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

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

[10] JEFFREYS H, 1935, MON NOT R ASTR SOC S, V3, P257