DEPTH OF SOURCE OF LEAD

[1] THORIUM IN STONE METEORITES BY NEUTRON ACTIVATION ANALYSIS [J]. GEOCHIMICA ET COSMOCHIMICA ACTA, 1959, 16 (1-3) : 88 - 100

[2] BULLEN KE, 1953, INTRODUCTION THEORY

[3] CONTENT OF LEAD IN EARTHS INITIAL CHONDRITE-LIKE OXIDE MASS + PARTITION COEFFICIENT OF LEAD FOR CRYSTALLIZATION OF SILICATE MELT [J]. NATURE, 1964, 203 (495) : 1161 - &

[4] RELATIVE DISTRIBUTION OF THORIUM URANIUM + LEAD ESTIMATED FROM ISOTOPIC COMPOSITION OF LEAD IN ORES [J]. NATURE, 1964, 203 (494) : 1062 - &

[5] MASUDA A, 1964, CHIGAKUZASSHI, V73, P139

[6] MASUDA A, 1964, INSJ, P65

[7] MASUDA A, IN PRESS

[8] MASUDA A, TO BE PUBLISHED

[9] MATSUMOTO T, 1963, J GEOSCI-OSAKA CITY, V7, P81

[1] THORIUM IN STONE METEORITES BY NEUTRON ACTIVATION ANALYSIS [J]. GEOCHIMICA ET COSMOCHIMICA ACTA, 1959, 16 (1-3) : 88 - 100

[2] BULLEN KE, 1953, INTRODUCTION THEORY

[3] CONTENT OF LEAD IN EARTHS INITIAL CHONDRITE-LIKE OXIDE MASS + PARTITION COEFFICIENT OF LEAD FOR CRYSTALLIZATION OF SILICATE MELT [J]. NATURE, 1964, 203 (495) : 1161 - &

[4] RELATIVE DISTRIBUTION OF THORIUM URANIUM + LEAD ESTIMATED FROM ISOTOPIC COMPOSITION OF LEAD IN ORES [J]. NATURE, 1964, 203 (494) : 1062 - &

[5] MASUDA A, 1964, CHIGAKUZASSHI, V73, P139

[6] MASUDA A, 1964, INSJ, P65

[7] MASUDA A, IN PRESS

[8] MASUDA A, TO BE PUBLISHED

[9] MATSUMOTO T, 1963, J GEOSCI-OSAKA CITY, V7, P81