东昆仑大格勒稀有金属矿化碳酸岩和橄榄岩斜锆石U-Pb年代学研究和找矿意义

王秉璋; 李五福; 金婷婷; 张晗; 李玉龙; 付长垒; 刘建栋; 王涛; 薛万文; 王泰山

doi:10.3799/dqkx.2022.280

Volume 49 Issue 4

Apr. 2024

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Article Navigation > Earth Science > 2024 > 49(4): 1245-1260

Wang Bingzhang, Li Wufu, Jin Tingting, Zhang Han, Li Yulong, Fu Changlei, Liu Jiandong, Wang Tao, Xue Wanwen, Wang Taishan, 2024. Baddeleyite U-Pb Geochronology of Rare Metal Mineralized Carbonatite and Peridotite in Dagele Area of East Kunlun Orogen and Its Prospecting Significance. Earth Science, 49(4): 1245-1260. doi: 10.3799/dqkx.2022.280

Citation:

Wang Bingzhang, Li Wufu, Jin Tingting, Zhang Han, Li Yulong, Fu Changlei, Liu Jiandong, Wang Tao, Xue Wanwen, Wang Taishan, 2024. Baddeleyite U-Pb Geochronology of Rare Metal Mineralized Carbonatite and Peridotite in Dagele Area of East Kunlun Orogen and Its Prospecting Significance. Earth Science, 49(4): 1245-1260. doi: 10.3799/dqkx.2022.280

Citation:

Wang Bingzhang, Li Wufu, Jin Tingting, Zhang Han, Li Yulong, Fu Changlei, Liu Jiandong, Wang Tao, Xue Wanwen, Wang Taishan, 2024. Baddeleyite U-Pb Geochronology of Rare Metal Mineralized Carbonatite and Peridotite in Dagele Area of East Kunlun Orogen and Its Prospecting Significance. Earth Science, 49(4): 1245-1260. doi: 10.3799/dqkx.2022.280

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Baddeleyite U-Pb Geochronology of Rare Metal Mineralized Carbonatite and Peridotite in Dagele Area of East Kunlun Orogen and Its Prospecting Significance

doi: 10.3799/dqkx.2022.280

1.
Qinghai Geological Survey Institute, Xining 810012, China
2.
Key Laboratory of the Northern Qinghai-Tibet Plateau Geological Processes and Mineral Resources, Xining 810012, China
3.
Engineering and Technology Center of Remote Sensing Big Data in Qinghai Province, Xining 810012, China
4.
Yanduzhongshi Geological Analysis Laboratories Ltd., Beijing 100094, China
5.
Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China

Received Date: 2022-04-18
Available Online: 2024-04-30
Publish Date: 2024-04-25

Abstract

Abstract

The rare-metal and rare-earth mineralized alkaline-carbonatite complex was first discovered in the Dagele area of East Kunlun orogen. This discovery indicates that the East Kunlun orogen has great prospects for rare-metal mineralization. Related studies are vital for understanding the geological processes and searching for rare-metal deposits in East Kunlun orogen. This study reports the geochemistry and geochronology of baddeleyites from peridotite and carbonatite within the Dagele alkaline complex. Baddeleyites from peridotite mainly contain ZrO₂ (96.48%-97.21%) with minor HfO₂ (0.83%-1.17%) and Nb₂O₅ (0.61%-0.93%). After common Pb correction using measured ²⁰⁷Pb, they yield weighted average ages of 381.0±2.3 Ma and 417.5±3.4 Ma with low intercept ages of 381.1±2.3 Ma and 417.7±3.4 Ma, respectively. Baddeleyites from carbonatite are mainly composed of ZrO₂ (91.1%), followed by HfO₂ (4.3%), Nb₂O₅ (1.22%), and FeO (2.31%). They yield weighted average ages of 381.5±2.5 Ma and 416.5±4.5 Ma with low intercept ages of 381.8±1.8 Ma and 416.7±4.5 Ma, respectively. It is inferred that the carbonatite and peridotite are formed at 381.8 Ma and 417.7 Ma, respectively. There are at least two stages of enrichment of Nb in the silica-unsaturated magma. Post-collisional and post-orogenic lithosphere extension and partial melting of mantle beneath the East Kunlun collisional orogen were considered as the geodynamic mechanism for its formation. Therefore, it is suggested that the Late Silurian-Devonian is an important period of rare-metal mineralization. The area between Dagela and Nuomuhong River is one of the important regions for prospecting of rare-metal mineralization.
- East Kunlun,
- Dagele,
- peridotite,
- carbonatite,
- baddeleyite,
- rare metals,
- geochemistry,
- petrology

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References(84)

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Baddeleyite U-Pb Geochronology of Rare Metal Mineralized Carbonatite and Peridotite in Dagele Area of East Kunlun Orogen and Its Prospecting Significance

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