Bai, Yingxiong; Shen, Ping; Cao, Chong; Li, Changhao; Feng, Haoxuan; Luo, Yaoqing; Pan, Hongdi; Suo, Qingyu (2023) In-situ elemental and boron isotopic variations of tourmaline from the Koktokay pegmatitic rare-metal deposit, China: Insights into external contamination and the source of the granitic pegmatite. Ore Geology Reviews, 162. doi:10.1016/j.oregeorev.2023.105683
| Reference Type | Journal (article/letter/editorial) | ||
|---|---|---|---|
| Title | In-situ elemental and boron isotopic variations of tourmaline from the Koktokay pegmatitic rare-metal deposit, China: Insights into external contamination and the source of the granitic pegmatite | ||
| Journal | Ore Geology Reviews | ||
| Authors | Bai, Yingxiong | Author | |
| Shen, Ping | Author | ||
| Cao, Chong | Author | ||
| Li, Changhao | Author | ||
| Feng, Haoxuan | Author | ||
| Luo, Yaoqing | Author | ||
| Pan, Hongdi | Author | ||
| Suo, Qingyu | Author | ||
| Year | 2023 (November) | Volume | 162 |
| Publisher | Elsevier BV | ||
| DOI | doi:10.1016/j.oregeorev.2023.105683Search in ResearchGate | ||
| Generate Citation Formats | |||
| Mindat Ref. ID | 16860612 | Long-form Identifier | mindat:1:5:16860612:4 |
| GUID | 0 | ||
| Full Reference | Bai, Yingxiong; Shen, Ping; Cao, Chong; Li, Changhao; Feng, Haoxuan; Luo, Yaoqing; Pan, Hongdi; Suo, Qingyu (2023) In-situ elemental and boron isotopic variations of tourmaline from the Koktokay pegmatitic rare-metal deposit, China: Insights into external contamination and the source of the granitic pegmatite. Ore Geology Reviews, 162. doi:10.1016/j.oregeorev.2023.105683 | ||
| Plain Text | Bai, Yingxiong; Shen, Ping; Cao, Chong; Li, Changhao; Feng, Haoxuan; Luo, Yaoqing; Pan, Hongdi; Suo, Qingyu (2023) In-situ elemental and boron isotopic variations of tourmaline from the Koktokay pegmatitic rare-metal deposit, China: Insights into external contamination and the source of the granitic pegmatite. Ore Geology Reviews, 162. doi:10.1016/j.oregeorev.2023.105683 | ||
| In | (2023) Ore Geology Reviews Vol. 162. Elsevier BV | ||
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