| Locality type: | Deposit |
| Classification |
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| Type: | Granite |
| Confirmation |
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| Validity: | Believed Valid |
| Data |
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| Mineral Data: | Click here to view Granite data |
| Locality Data: | Click here to view Shulouqiu U deposit (U deposit No. 302), Changjiang Uranium ore field (Uranium ore field No. 211), Renhua Co., Shaoguan, Guangdong, China |
| Data Identifiers |
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| Mindat Occurrence Record ID: | 1651755 |
| Long-form Identifier: | 1:3:1651755:6 |
| GUID (UUID V4): | 0 |
| Nearest other occurrences of Granite |
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| 16.2km (10.0 miles) | ⓘSanjiu Ore Field, Rucheng Co., Chenzhou, Hunan, China |
| 20.3km (12.6 miles) | ⓘMianhuakeng U deposit (U deposit No. 305), Changjiang Uranium ore field (Uranium ore field No. 211), Renhua Co., Shaoguan, Guangdong, China |
| 22.1km (13.8 miles) | ⓘLanhe deposit (U deposit No. 201), Baishun Uranium ore field, Nanxiong Co., Shaoguan, Guangdong, China |
| 31.6km (19.6 miles) | ⓘTiemuli W–Fe skarn-type deposit, Chongyi Co., Ganzhou, Jiangxi, China |
| 34.3km (21.3 miles) | ⓘAotou Sn deposit, Jiulongnao W-Sn ore field, Dayu Co., Ganzhou, Jiangxi, China |
| 34.5km (21.4 miles) | ⓘYangjiaonao U deposit, Lujing Uranium ore field, Chongyi Co., Ganzhou, Jiangxi, China |
| 37.1km (23.0 miles) | ⓘXiaoshan U deposit, Lujing Uranium ore field, Chongyi Co., Ganzhou, Jiangxi, China |
| 37.4km (23.2 miles) | ⓘLujing deposit (Sanerer deposit; U deposit No. 322), Lujing Uranium ore field, Chongyi Co., Ganzhou, Jiangxi, China |
| 39.2km (24.4 miles) | ⓘGaoaobei W-Li deposit, Chongyi Co., Ganzhou, Jiangxi, China |
| 41.0km (25.5 miles) | ⓘTutianmen W deposit, Baiyunxian W-polymetallic ore field, Rucheng Co., Chenzhou, Hunan, China |
| References |
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Gao, Shen; Wang, Yongjian; Zou, Xinyu; Vinis, Edward L.; Huang, Liangliang; Tao, Yi; Xu, Jing; Qin, Kezhang; Qiu, Zhengjie (2024) Fluid overprints and mineralization of the Zhuguangshan granite-related U district in China: Recorded by cathodoluminescence textures and chemistry of quartz. Ore Geology Reviews, 173. doi:10.1016/j.oregeorev.2024.106256 |
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