THE CHEMICAL CLASSIFICATION OF IRON METEORITES. I. A STUDY OF IRON METEORITES WITH LOW CONCENTRATIONS OF GALLIUM AND GERMANIUM.
THE CHEMICAL CLASSIFICATION OF IRON METEORITES. I. A STUDY OF IRON METEORITES WITH LOW CONCENTRATIONS OF GALLIUM AND GERMANIUM.
复制标题
铁陨石的化学分类。
DOI:
10.1016/s0016-7037(67)80043-7
复制
发表时间:
1967
影响因子:
5
通讯作者:
J. Wasson
中科院分区:
文献类型:
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作者:
J. Wasson
The concentrations of Ga and Ge have been determined in 34 iron meteorites. The meteorites were chosen either because they were found to have Ga or Ge concentrations below the detection limits of previous investigators, or because they were similar in structure and Ni content to meteorites of the former sort. All but 3 of the meteorites belong to one of the following two classes: ataxites with greater than 13% Ni, or fine octahedrites with less than 9·5% Ni. On the basis of the new results it is possible to resolve Gasingle bondGe group IV ofLoveringet al.(1957) into two distinct groups, designated Gasingle bondGe groups IVa and IVb, and having 12 and 6 members respectively. Three meteorites have Ga and Ge concentrations similar to meteorites in Group III, whereas the remaining 13 meteorites cannot be assigned to any of the known Gasingle bondGe groups. Certain regularities are to be seen in plots of Ge vs. Ga concentration and Ge vs. Ni concentration. These are discussed in terms of the multiple parent-body hypothesis and also in terms of planetary fractionation processes. Evidence is discussed which indicates that Gasingle bondGe groups I, IVa and possibly IVb represent fully resolved groups, whereas the remaining groups are complex. An attempt at resolving the latter groups on the basis of detailed chemical studies is proposed.
DOI:
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发表时间:
2007
期刊:
Lunar and Planetary Science Conference XXXVIII 38
影响因子:
--
作者:
原田 知明;保科 洋介;吉村 英恭;C.Okamoto
通讯作者:
C.Okamoto