RANGE OF EARTH STRUCTURE NONUNIQUENESS IMPLIED BY BODY WAVE OBSERVATIONS

[1] ANDERSON DL, 1972, GEOL SOC AM ABSTR, V4, P123

[2] ANTONOVA LM, 1971, ALGORITHMS INTERPRET, P260

[3] ARCHAMBEAU CB, 1966, 142 SEISM DAT LAB

[4] UNIQUENESS IN INVERSION OF INACCURATE GROSS EARTH DATA [J]. PHILOSOPHICAL TRANSACTIONS OF THE ROYAL SOCIETY OF LONDON SERIES A-MATHEMATICAL AND PHYSICAL SCIENCES, 1970, 266 (1173) : 123 - &

[5] RESOLVING POWER OF GROSS EARTH DATA [J]. GEOPHYSICAL JOURNAL OF THE ROYAL ASTRONOMICAL SOCIETY, 1968, 16 (02): : 169 - &

[6] INFERENCE FROM INADEQUATE AND INACCURATE DATA, III [J]. PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA, 1970, 67 (01) : 282 - +

[7] BACKUS G, 1970, P NATL ACAD SCI USA, V65, P1, DOI 10.1073/pnas.65.1.1

[8] NUMERICAL APPLICATIONS OF A FORMALISM FOR GEOPHYSICAL INVERSE PROBLEMS [J]. GEOPHYSICAL JOURNAL OF THE ROYAL ASTRONOMICAL SOCIETY, 1967, 13 (1-3): : 247 - &

[9] Bateman H, 1910, PHYS Z, V11, P96

[10] The solution of the integral equation connecting the velocity of propagation of an earthquake-wave in the interior of the Earth with the times which the disturbance takes to travel to the different stations on the Earth's surface. [J]. PHILOSOPHICAL MAGAZINE, 1910, 19 (109-14) : 576 - 587

[1] ANDERSON DL, 1972, GEOL SOC AM ABSTR, V4, P123

[2] ANTONOVA LM, 1971, ALGORITHMS INTERPRET, P260

[3] ARCHAMBEAU CB, 1966, 142 SEISM DAT LAB

[4] UNIQUENESS IN INVERSION OF INACCURATE GROSS EARTH DATA [J]. PHILOSOPHICAL TRANSACTIONS OF THE ROYAL SOCIETY OF LONDON SERIES A-MATHEMATICAL AND PHYSICAL SCIENCES, 1970, 266 (1173) : 123 - &

[5] RESOLVING POWER OF GROSS EARTH DATA [J]. GEOPHYSICAL JOURNAL OF THE ROYAL ASTRONOMICAL SOCIETY, 1968, 16 (02): : 169 - &

[6] INFERENCE FROM INADEQUATE AND INACCURATE DATA, III [J]. PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA, 1970, 67 (01) : 282 - +

[7] BACKUS G, 1970, P NATL ACAD SCI USA, V65, P1, DOI 10.1073/pnas.65.1.1

[8] NUMERICAL APPLICATIONS OF A FORMALISM FOR GEOPHYSICAL INVERSE PROBLEMS [J]. GEOPHYSICAL JOURNAL OF THE ROYAL ASTRONOMICAL SOCIETY, 1967, 13 (1-3): : 247 - &

[9] Bateman H, 1910, PHYS Z, V11, P96

[10] The solution of the integral equation connecting the velocity of propagation of an earthquake-wave in the interior of the Earth with the times which the disturbance takes to travel to the different stations on the Earth's surface. [J]. PHILOSOPHICAL MAGAZINE, 1910, 19 (109-14) : 576 - 587