月岩的穆斯堡尔谱学研究 |
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引用本文: | 计桂泉,吴卫芳,李士,宗普和.月岩的穆斯堡尔谱学研究[J].地球化学,1981(2):158-161. |
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作者姓名: | 计桂泉 吴卫芳 李士 宗普和 |
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作者单位: | [1]中国科学院地球化学研究所 [2]中国科学院高能物理研究所 |
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摘 要: | The results of Moessbauer study of Apollo-17 Mare basalt are reported in this paper.It has been revealed that Fe in iron.bearing minerals in the basalt is almost present in the form of Fe^3 , with Fe^3 less than 3% of total iron. The site occupancy of Fe^3 ions at M1 and M2 is approximately 0.3 and the corresponding equilibrium constant K (T) is about 0.06, thus indicating that the mare basalt is formed through crystallization under high-temperature reducing and rather slow cooling conditions.
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关 键 词: | 月岩 穆斯堡尔谱 玄武岩 单斜 |
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