Hsu & Sabatini (2019) — 5,886 geological ore samples
5886 samples found (page 38/118)
| Sample No. | Specimen | Site (English) | Admin Province | Metal Province | Metal Type | ²⁰⁶Pb/²⁰⁴Pb | ²⁰⁷Pb/²⁰⁴Pb | ²⁰⁸Pb/²⁰⁴Pb | Quality | Reference |
|---|---|---|---|---|---|---|---|---|---|---|
| galena | Baiyangfan | Jiangxi | Lower Yangtze | Ag-Pb-Zn | 17.9894 | 15.5927 | 38.3817 | Good | 鍾浩.2016.江西九瑞矿集区白杨畈铅锌银矿床硫化物硫铅同位素及微量元素特征.江西地質17(3): 152-159 | |
| galena | Baiyangfan | Jiangxi | Lower Yangtze | Ag-Pb-Zn | 17.9813 | 15.5869 | 38.3580 | Good | 鍾浩.2016.江西九瑞矿集区白杨畈铅锌银矿床硫化物硫铅同位素及微量元素特征.江西地質17(3): 152-159 | |
| galena | Baiyangfan | Jiangxi | Lower Yangtze | Ag-Pb-Zn | 17.9817 | 15.5866 | 38.3625 | Good | 鍾浩.2016.江西九瑞矿集区白杨畈铅锌银矿床硫化物硫铅同位素及微量元素特征.江西地質17(3): 152-159 | |
| galena | Baiyangfan | Jiangxi | Lower Yangtze | Ag-Pb-Zn | 17.9894 | 15.5913 | 38.3725 | Good | 鍾浩.2016.江西九瑞矿集区白杨畈铅锌银矿床硫化物硫铅同位素及微量元素特征.江西地質17(3): 152-159 | |
| 1 | galena | Yinshan | Jiangxi | Lower Yangtze | Polymetallic | 19.0460 | 16.3680 | 40.2370 | Bad | 何国朝.1992.江西银山矿床的稳定同位素组成特征.礦產與地質6(5): 406-411 |
| 2 | galena | Yinshan | Jiangxi | Lower Yangtze | Polymetallic | 17.8890 | 15.4580 | 37.6860 | Bad | 何国朝.1992.江西银山矿床的稳定同位素组成特征.礦產與地質6(5): 406-411 |
| 3 | galena | Yinshan | Jiangxi | Lower Yangtze | Polymetallic | 17.9840 | 15.5100 | 37.8930 | Bad | 何国朝.1992.江西银山矿床的稳定同位素组成特征.礦產與地質6(5): 406-411 |
| 4 | galena | Yinshan | Jiangxi | Lower Yangtze | Polymetallic | 17.9580 | 15.5030 | 37.9110 | Bad | 何国朝.1992.江西银山矿床的稳定同位素组成特征.礦產與地質6(5): 406-411 |
| 5 | galena | Yinshan | Jiangxi | Lower Yangtze | Polymetallic | 18.0050 | 15.5730 | 38.1540 | Bad | 何国朝.1992.江西银山矿床的稳定同位素组成特征.礦產與地質6(5): 406-411 |
| 6 | galena | Yinshan | Jiangxi | Lower Yangtze | Polymetallic | 18.0100 | 15.5450 | 38.0220 | Bad | 何国朝.1992.江西银山矿床的稳定同位素组成特征.礦產與地質6(5): 406-411 |
| 7 | galena | Yinshan | Jiangxi | Lower Yangtze | Polymetallic | 17.9670 | 15.5170 | 37.9070 | Bad | 何国朝.1992.江西银山矿床的稳定同位素组成特征.礦產與地質6(5): 406-411 |
| 8 | galena | Yinshan | Jiangxi | Lower Yangtze | Polymetallic | 17.9270 | 15.4660 | 37.8180 | Bad | 何国朝.1992.江西银山矿床的稳定同位素组成特征.礦產與地質6(5): 406-411 |
| 9 | galena | Yinshan | Jiangxi | Lower Yangtze | Polymetallic | 18.0730 | 15.7550 | 37.9920 | Bad | 何国朝.1992.江西银山矿床的稳定同位素组成特征.礦產與地質6(5): 406-411 |
| 10 | galena | Yinshan | Jiangxi | Lower Yangtze | Polymetallic | 17.9560 | 15.4590 | 37.7350 | Bad | 何国朝.1992.江西银山矿床的稳定同位素组成特征.礦產與地質6(5): 406-411 |
| 11 | galena | Yinshan | Jiangxi | Lower Yangtze | Polymetallic | 18.2040 | 15.7550 | 38.4070 | Bad | 何国朝.1992.江西银山矿床的稳定同位素组成特征.礦產與地質6(5): 406-411 |
| 12 | galena | Yinshan | Jiangxi | Lower Yangtze | Polymetallic | 18.0140 | 15.5170 | 37.9230 | Bad | 何国朝.1992.江西银山矿床的稳定同位素组成特征.礦產與地質6(5): 406-411 |
| 13 | galena | Yinshan | Jiangxi | Lower Yangtze | Polymetallic | 18.0930 | 15.5920 | 38.2640 | Bad | 何国朝.1992.江西银山矿床的稳定同位素组成特征.礦產與地質6(5): 406-411 |
| 14 | galena | Yinshan | Jiangxi | Lower Yangtze | Polymetallic | 18.0050 | 15.5120 | 37.9460 | Bad | 何国朝.1992.江西银山矿床的稳定同位素组成特征.礦產與地質6(5): 406-411 |
| galena | Wushan | Jiangxi | Lower Yangtze | Cu-Au | 17.8800 | 15.5380 | 38.1510 | Bad | 季紹新1990.節錄於李文达等1998.中国东南部中生代火成岩与矿床 | |
| galena | Wushan | Jiangxi | Lower Yangtze | Cu-Au | 17.8860 | 15.4990 | 38.0260 | Bad | 季紹新1990.節錄於李文达等1998.中国东南部中生代火成岩与矿床 | |
| galena | Wushan | Jiangxi | Lower Yangtze | Cu-Au | 17.9130 | 15.5260 | 38.1300 | Bad | 季紹新1990.節錄於李文达等1998.中国东南部中生代火成岩与矿床 | |
| galena | Wushan | Jiangxi | Lower Yangtze | Cu-Au | 17.8900 | 15.4900 | 38.0400 | Bad | 季紹新1990.節錄於李文达等1998.中国东南部中生代火成岩与矿床 | |
| galena | Chengmenshan | Jiangxi | Lower Yangtze | Cu | 18.4000 | 15.6500 | 39.0500 | Bad | 季紹新1990.節錄於李文达等1998.中国东南部中生代火成岩与矿床 | |
| galena | Wushan | Jiangxi | Lower Yangtze | Cu-Au | 17.8800 | 15.5100 | 38.1200 | Bad | 季紹新1990.節錄於李文达等1998.中国东南部中生代火成岩与矿床 | |
| feldspar | Tongchang | Jiangxi | Lower Yangtze | Cu | 18.0550 | 15.5460 | 38.1170 | Bad | 季紹新1990.節錄於李文达等1998.中国东南部中生代火成岩与矿床 | |
| feldspar | Yangchuling | Jiangxi | Lower Yangtze | Mo-W | 18.3560 | 15.6150 | 38.4050 | Bad | 季紹新1990.節錄於李文达等1998.中国东南部中生代火成岩与矿床 | |
| galena | Dongxiang | Jiangxi | Lower Yangtze | Polymetallic | 17.7420 | 15.5890 | 38.3940 | Bad | 季紹新1990.節錄於李文达等1998.中国东南部中生代火成岩与矿床 | |
| galena | Qibaoshan | Jiangxi | Lower Yangtze | Polymetallic | 17.7280 | 15.5070 | 37.9130 | Bad | 季紹新1990.節錄於李文达等1998.中国东南部中生代火成岩与矿床 | |
| galena | Yinshan | Jiangxi | Lower Yangtze | Polymetallic | 18.0520 | 15.4320 | 37.6550 | Bad | 季紹新1990.節錄於李文达等1998.中国东南部中生代火成岩与矿床 | |
| galena | Songping | Jiangxi | Lower Yangtze | Polymetallic | 18.1710 | 15.5490 | 38.3100 | Bad | 季紹新1990.節錄於李文达等1998.中国东南部中生代火成岩与矿床 | |
| 2 | galena | Chengmenshan | Jiangxi | Lower Yangtze | Cu | 18.6070 | 15.9290 | 39.2900 | Bad | 孟良义.1988.城门山铜、钼矿床的稳定同位素地质.長春地質學院院報18(3): 268-276, 304 |
| 3 | feldspar | Chengmenshan | Jiangxi | Lower Yangtze | Cu | 18.0420 | 15.5720 | 37.9330 | Bad | 孟良义.1988.城门山铜、钼矿床的稳定同位素地质.長春地質學院院報18(3): 268-276, 304 |
| 4 | feldspar | Chengmenshan | Jiangxi | Lower Yangtze | Cu | 18.8330 | 15.7200 | 37.8140 | Bad | 孟良义.1988.城门山铜、钼矿床的稳定同位素地质.長春地質學院院報18(3): 268-276, 304 |
| galena | Cunqian | Jiangxi | Lower Yangtze | Polymetallic | 17.8830 | 15.4980 | 38.5670 | Good | 王強.2013.江西省村前铜多金属矿床含矿岩体地球化学特征及矿床成因研究.成都理工大學碩士論文 | |
| galena | Cunqian | Jiangxi | Lower Yangtze | Polymetallic | 18.0370 | 15.6500 | 39.0170 | Good | 王強.2013.江西省村前铜多金属矿床含矿岩体地球化学特征及矿床成因研究.成都理工大學碩士論文 | |
| galena | Cunqian | Jiangxi | Lower Yangtze | Polymetallic | 18.0270 | 15.6680 | 39.0890 | Good | 王強.2013.江西省村前铜多金属矿床含矿岩体地球化学特征及矿床成因研究.成都理工大學碩士論文 | |
| galena | Cunqian | Jiangxi | Lower Yangtze | Polymetallic | 18.1100 | 15.7200 | 39.2000 | Good | 王強.2013.江西省村前铜多金属矿床含矿岩体地球化学特征及矿床成因研究.成都理工大學碩士論文 | |
| 42 (w35) | galena | Wushan | Jiangxi | Lower Yangtze | Cu-Au | 17.8820 | 15.5000 | 38.0790 | Bad | Huang et al. 1990. Reported by Pan & Dong.1999. The Lower Changjiang metallogenic belt. Ore Geology Reviews 15: 177-242 |
| 43 (G18) | galena | Wushan | Jiangxi | Lower Yangtze | Cu-Au | 18.3800 | 15.6300 | 39.1300 | Bad | Huang et al. 1990. Reported by Pan & Dong.1999. The Lower Changjiang metallogenic belt. Ore Geology Reviews 15: 177-242 |
| 46 (w125) | galena | Wushan | Jiangxi | Lower Yangtze | Cu-Au | 17.8800 | 15.4900 | 38.0400 | Bad | Huang et al. 1990. Reported by Pan & Dong.1999. The Lower Changjiang metallogenic belt. Ore Geology Reviews 15: 177-242 |
| 61 (w34) | feldspar | Wushan | Jiangxi | Lower Yangtze | Cu-Au | 17.9540 | 15.5360 | 38.1310 | Bad | Ji et al. 1990. Reported by Pan & Dong.1999. The Lower Changjiang metallogenic belt. Ore Geology Reviews 15: 177-242 |
| 63 (G18) | galena | Yangjishan | Jiangxi | Lower Yangtze | Au | 18.0700 | 15.5280 | 38.0760 | Bad | Ji et al. 1990. Reported by Pan & Dong.1999. The Lower Changjiang metallogenic belt. Ore Geology Reviews 15: 177-242 |
| FH-48 | galena | Fenghuangshan | Anhui | Lower Yangtze | Cu | 18.5310 | 15.6230 | 38.6320 | Good | 瞿泓滢 2010 安徽铜陵凤凰山矽卡岩型铜矿床成矿过程研究.中國地質科學院博士論文 |
| FH-100 | galena | Fenghuangshan | Anhui | Lower Yangtze | Cu | 18.5640 | 15.6210 | 38.6260 | Good | 瞿泓滢 2010 安徽铜陵凤凰山矽卡岩型铜矿床成矿过程研究.中國地質科學院博士論文 |
| DH001 | galena | Dishuiya | Anhui | Lower Yangtze | Polymetallic | 18.4300 | 15.8700 | 39.9100 | Bad | 陈毓蔚1980.我国显生代金属矿床铅同位素 组成特征及其成因探讨.地球化學3: 215-229 |
| V001 | galena | Huangshanling | Anhui | Lower Yangtze | Polymetallic | 18.0500 | 15.4100 | 38.0100 | Bad | 陈毓蔚1980.我国显生代金属矿床铅同位素 组成特征及其成因探讨.地球化學3: 215-229 |
| V002 | galena | Hengshanyou | Anhui | Lower Yangtze | Polymetallic | 18.5500 | 15.9300 | 39.7100 | Bad | 陈毓蔚1980.我国显生代金属矿床铅同位素 组成特征及其成因探讨.地球化學3: 215-229 |
| V003 | galena | Xueshuifu | Anhui | Lower Yangtze | Polymetallic | 17.9600 | 15.3000 | 37.6800 | Bad | 陈毓蔚1980.我国显生代金属矿床铅同位素 组成特征及其成因探讨.地球化學3: 215-229 |
| 孟-1 | galena | Qingyang | Anhui | Lower Yangtze | Polymetallic | 18.3300 | 15.6400 | 38.1200 | Bad | 陈毓蔚1980.我国显生代金属矿床铅同位素 组成特征及其成因探讨.地球化學3: 215-229 |
| 程-1 | galena | Qingyang | Anhui | Lower Yangtze | Polymetallic | 18.2800 | 15.5600 | 38.1600 | Bad | 陈毓蔚1980.我国显生代金属矿床铅同位素 组成特征及其成因探讨.地球化學3: 215-229 |