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机译:独特achondrite西北非洲6704的起源:来自岩石,化学和re-OS,O和Ti同位素系统的限制
Univ Tokyo Dept Earth &
Planetary Sci Bunkyo Ku Hongo 7-3-1 Tokyo 1130033 Japan;
Univ Maryland Dept Geol College Pk MD 20742 USA;
Okayama Univ IPM Pheast Mem Lab Geochem &
Cosmochem Misasa Tottori 6820193 Japan;
Univ Calif Davis Dept Earth &
Planetary Sci One Shields Ave Davis CA 95616 USA;
Tohoku Univ Grad Sch Sci Div Earth &
Planetary Mat Sci Lab Early Solar Syst Evolut Aoba Ku Sendai Miyagi Japan;
Univ Tokyo Dept Earth &
Planetary Sci Bunkyo Ku Hongo 7-3-1 Tokyo 1130033 Japan;
Univ Tokyo Dept Earth &
Planetary Sci Bunkyo Ku Hongo 7-3-1 Tokyo 1130033 Japan;
Univ Maryland Dept Geol College Pk MD 20742 USA;
Natl Inst Polar Res 10-3 Midori Cho Tachikawa Tokyo 1908518 Japan;
Univ Calif Davis Dept Earth &
Planetary Sci One Shields Ave Davis CA 95616 USA;
Tohoku Univ Grad Sch Sci Div Earth &
Planetary Mat Sci Lab Early Solar Syst Evolut Aoba Ku Sendai Miyagi Japan;
Univ Washington Dept Earth &
Space Sci Seattle WA 98195 USA;
NWA 6704; Primitive achondrite; Nucleosynthetic anomalies; Highly siderophile elements; Impact melting;
机译:独特achondrite西北非洲6704的起源:来自岩石,化学和re-OS,O和Ti同位素系统的限制
机译:独特的玄武质长晶陨石在非洲西北部2976由Al-Mg和U-Pb同位素系统对早期太阳系年表的新限制
机译:从岩石,微量元素,氧气,铬和钛同位素和中红外光谱法中取出未分组的Achondrite西北非洲7325的培养和出处
机译:SM-ND,RB-SR,K-AR和RE-OS同位素约束对Konder MaseIF,Khabarov地区,俄罗斯Konder Mineization的起源。
机译:大陆岩石圈地幔的起源,演化和消亡:Re-Os同位素,地球化学,岩石学和模型学的观点。
机译:岩石学痕量元素氧铬和钛同位素以及中红外光谱法对西北非洲无群陨石7325的岩石成因和物源
机译:U-Pb,RB-SR和AR-AR系统的未分组Achondrites西北非洲6704和西北非洲6693