Ruby–bearing feldspathic dike in peridotite from Ray–Iz ophiolite, the Polar Urals: Implications for mantle metasomatism and origin of ruby
Ruby–bearing feldspathic dike in peridotite from Ray–Iz ophiolite, the Polar Urals: Implications for mantle metasomatism and origin of ruby
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DOI：
10.2465/jmps.141021
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发表时间：
2015
影响因子：
0.7
通讯作者：
S. Ishimaru;S. Arai;M. Miura;V. Shmelev;E. Pushkarev
中科院分区：
文献类型：
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作者：
S. Ishimaru;S. Arai;M. Miura;V. Shmelev;E. Pushkarev
* 熊本大学科学技术研究生院地球与环境科学系，2-39-1 Kurokami，Chuo-ku，Kumamoto 860-8555，Japan ** 金泽大学地球科学系，Kakuma，Kanazawa 920-1192，Japan ***ODS，JAMSTEC，2-15 Natsushima，Yokosuka 237-0061，Japan Zavaritskii Institute of Geology and Geochemistry，俄罗斯科学院乌拉尔分支
*Department of Earth and Environmental Sciences, Graduate School of Science and Technology, Kumamoto University, 2–39–1 Kurokami, Chuo–ku, Kumamoto 860–8555, Japan **Department of Earth Sciences, Kanazawa University, Kakuma, Kanazawa 920–1192, Japan ***ODS, JAMSTEC, 2–15 Natsushima, Yokosuka 237–0061, Japan Zavaritskii Institute of Geology and Geochemistry, Ural Branch, Russian Academy of Sciences, Russia