GEOCHRONOLOGY BY RADIOACTIVE DECAY

[1] IMPLICATIONS OF THE RHODESIA AGE PATTERN [J]. GEOCHIMICA ET COSMOCHIMICA ACTA, 1955, 8 (1-2) : 1 - 15

[2] THE CONVERGENT LEAD AGES OF THE OLDEST MONAZITES AND URANINITES (RHODESIA, MANITOBA, MADAGASCAR, AND TRANSVAAL) [J]. GEOCHIMICA ET COSMOCHIMICA ACTA, 1955, 7 (5-6) : 294 - 299

[3] THE RADIOACTIVE DECAY CONSTANTS OF K-40 AS DETERMINED FROM THE ACCUMULATION OF CA-40 IN ANCIENT MINERALS [J]. PHYSICAL REVIEW, 1948, 74 (03): : 279 - 286

[4] AHRENS LH, 1956, PHYS CHEM EARTH, V1, P44

[5] HALF-LIFE OF RB-87 [J]. PHYSICAL REVIEW, 1956, 103 (04): : 1045 - 1047

[6] RADIOACTIVE AGES OF MINERALS FROM THE BROWN DERBY MINE AND THE QUARTZ CREEK GRANITE NEAR GUNNISON, COLORADO [J]. JOURNAL OF GEOPHYSICAL RESEARCH, 1956, 61 (02): : 215 - 232

[7] ALDRICH LT, 1956, GEOCHIM COSMOCHIM AC, V10, P238

[8] MEASUREMENT OF RADIOACTIVE AGES OF ROCKS [J]. SCIENCE, 1956, 123 (3203) : 871 - 875

[9] ALDRICH LT, 1957, B GEOL SOC AMER, V68, P655

[10] BERYLLIUM-10 PRODUCED BY COSMIC RAYS [J]. SCIENCE, 1956, 124 (3222) : 584 - 585

[1] IMPLICATIONS OF THE RHODESIA AGE PATTERN [J]. GEOCHIMICA ET COSMOCHIMICA ACTA, 1955, 8 (1-2) : 1 - 15

[2] THE CONVERGENT LEAD AGES OF THE OLDEST MONAZITES AND URANINITES (RHODESIA, MANITOBA, MADAGASCAR, AND TRANSVAAL) [J]. GEOCHIMICA ET COSMOCHIMICA ACTA, 1955, 7 (5-6) : 294 - 299

[3] THE RADIOACTIVE DECAY CONSTANTS OF K-40 AS DETERMINED FROM THE ACCUMULATION OF CA-40 IN ANCIENT MINERALS [J]. PHYSICAL REVIEW, 1948, 74 (03): : 279 - 286

[4] AHRENS LH, 1956, PHYS CHEM EARTH, V1, P44

[5] HALF-LIFE OF RB-87 [J]. PHYSICAL REVIEW, 1956, 103 (04): : 1045 - 1047

[6] RADIOACTIVE AGES OF MINERALS FROM THE BROWN DERBY MINE AND THE QUARTZ CREEK GRANITE NEAR GUNNISON, COLORADO [J]. JOURNAL OF GEOPHYSICAL RESEARCH, 1956, 61 (02): : 215 - 232

[7] ALDRICH LT, 1956, GEOCHIM COSMOCHIM AC, V10, P238

[8] MEASUREMENT OF RADIOACTIVE AGES OF ROCKS [J]. SCIENCE, 1956, 123 (3203) : 871 - 875

[9] ALDRICH LT, 1957, B GEOL SOC AMER, V68, P655

[10] BERYLLIUM-10 PRODUCED BY COSMIC RAYS [J]. SCIENCE, 1956, 124 (3222) : 584 - 585