Content of Lead in the Earth's Initial Chondrite-like Oxide Mass and the Partition Coefficient of Lead for Crystallization of Silicate Melt-Reference-Cited by-同舟云学术

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Content of Lead in the Earth's Initial Chondrite-like Oxide Mass and the Partition Coefficient of Lead for Crystallization of Silicate Melt

Published:1964-09 Issue:4950 Volume:203 Page:1161-1162
ISSN:0028-0836
Container-title:Nature
language:en
Short-container-title:Nature

Author:

MASUDA AKIMASA

Publisher

Springer Science and Business Media LLC

Subject

Multidisciplinary

Link

http://www.nature.com/articles/2031161a0.pdf

Reference12 articles.

1. Masuda, A., Nature, 203, 1062 (1964).

2. Masuda, A., and Matsui, Y., INSJ-53, Inst. Nucl. Study, Univ. Tokyo (1963).

3. Masuda, A., and Matsui, Y., Geochim. Cosmochim. Acta (in the press).

4. Masuda, A., Chigaku-zasshi, 73, 139 (1964).

5. Masuda, A., INSJ-65, Inst. Nucl. Study, Univ. Tokyo (1964).

Cited by 12 articles. 订阅此论文施引文献订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献

1. Determination of REE, Ba, Fe, Mg, Na and K in carbonaceous and ordinary chondrites;Geochimica et Cosmochimica Acta;1974-05

2. CHROMATOGRAPHIC ANALYSIS;Molten Salts Handbook;1967

3. The difference in lanthanide abundance pattern between the crust and the chondrite and its possible meaning to the genesis of crust and mantle;Geochimica et Cosmochimica Acta;1966-02

4. Genesis of the earth's crust and the structure within the mantle: A unified chemical theory;Chemical Geology;1966

5. A geochemical coincidence between strontium isotopes and lead isotopes;Chemical Geology;1966

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