| Origin of middle Miocene leucogranites and rhyolites on the Tibetan Plateau: Constraints on the timing of crustal thickening and uplift of its northern boundary | |
| Zhang LY (张利云); Ding L (丁林); Yang D (杨迪); Xu Q (许强); Cai FL (蔡福龙); Liu DL (刘德亮); Ding, L (通讯作者),Chinese Acad Sci, Inst Tibetan Plateau Res, Key Lab Continental Collis & Plateau Uplift, Beijing 100085, Peoples R China. | |
| Source Publication | CHINESE SCIENCE BULLETIN
 |
| 2012 | |
| Volume | 57Issue:5Pages:511-524 |
| Subject Area | 地质学 |
| WOS ID | WOS:000299924000012 |
| Language | 英语 |
| Indexed By | SCI |
| Keyword | India-asia Collision East-west Extension Yardoi Gneiss Dome Ulugh-muztagh Area Kunlun Fault Zone Southern Tibet Volcanic-rocks Himalayan Leukogranites Geochemical Constraints Geological Implications |
| Cooperation Status | 国内 |
| Citation statistics | |
| Document Type | 期刊论文 |
| Identifier | http://ir.itpcas.ac.cn/handle/131C11/2143 |
| Collection | 图书馆 |
| Corresponding Author | Ding, L (通讯作者),Chinese Acad Sci, Inst Tibetan Plateau Res, Key Lab Continental Collis & Plateau Uplift, Beijing 100085, Peoples R China. |
| Recommended Citation GB/T 7714 | Zhang LY ,Ding L ,Yang D ,et al. Origin of middle Miocene leucogranites and rhyolites on the Tibetan Plateau: Constraints on the timing of crustal thickening and uplift of its northern boundary[J]. CHINESE SCIENCE BULLETIN,2012,57(5):511-524. |
| APA | Zhang LY .,Ding L .,Yang D .,Xu Q .,Cai FL .,...&Ding, L .(2012).Origin of middle Miocene leucogranites and rhyolites on the Tibetan Plateau: Constraints on the timing of crustal thickening and uplift of its northern boundary.CHINESE SCIENCE BULLETIN,57(5),511-524. |
| MLA | Zhang LY ,et al."Origin of middle Miocene leucogranites and rhyolites on the Tibetan Plateau: Constraints on the timing of crustal thickening and uplift of its northern boundary".CHINESE SCIENCE BULLETIN 57.5(2012):511-524. |
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| File Name/Size | DocType | Version | Access | License | ||
| V.57(5) 511-524 2012（1640KB） | 开放获取 | License | View Application Full Text | |||
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