Hsu & Sabatini (2019) — 5,886 geological ore samples
5886 samples found (page 41/118)
| Sample No. | Specimen | Site (English) | Admin Province | Metal Province | Metal Type | ²⁰⁶Pb/²⁰⁴Pb | ²⁰⁷Pb/²⁰⁴Pb | ²⁰⁸Pb/²⁰⁴Pb | Quality | Reference |
|---|---|---|---|---|---|---|---|---|---|---|
| 24 | galena | Tongguanshan | Anhui | Lower Yangtze | Polymetallic | 18.3200 | 15.5300 | 38.7500 | Bad | 黄许陈.1994.安徽省铜陵地区成矿物质和含矿流体来源问题的探讨.安徽地質3 |
| 25 | galena | Tongguanshan | Anhui | Lower Yangtze | Polymetallic | 18.3500 | 15.6000 | 38.0500 | Bad | 黄许陈.1994.安徽省铜陵地区成矿物质和含矿流体来源问题的探讨.安徽地質3 |
| 26 | galena | Tongguanshan | Anhui | Lower Yangtze | Polymetallic | 19.3300 | 16.4500 | 40.7400 | Bad | 黄许陈.1994.安徽省铜陵地区成矿物质和含矿流体来源问题的探讨.安徽地質3 |
| 27 | galena | Tongguanshan | Anhui | Lower Yangtze | Polymetallic | 18.5400 | 16.0200 | 39.6200 | Bad | 黄许陈.1994.安徽省铜陵地区成矿物质和含矿流体来源问题的探讨.安徽地質3 |
| Y-1 | feldspar | Xinqiao | Anhui | Lower Yangtze | Polymetallic | 18.4210 | 15.4880 | 38.1510 | Good | 臧文拴.2007.浅析安徽省新桥S-Fe矿田的成因.矿床地質26(4): 464-474 |
| Y-2 | feldspar | Xinqiao | Anhui | Lower Yangtze | Polymetallic | 18.3630 | 15.5120 | 38.2250 | Good | 臧文拴.2007.浅析安徽省新桥S-Fe矿田的成因.矿床地質26(4): 464-474 |
| Y-3 | feldspar | Xinqiao | Anhui | Lower Yangtze | Polymetallic | 18.2730 | 15.4820 | 38.0900 | Good | 臧文拴.2007.浅析安徽省新桥S-Fe矿田的成因.矿床地質26(4): 464-474 |
| galena | Laoyaling | Anhui | Lower Yangtze | Polymetallic | 17.8800 | 15.2230 | 36.7020 | Bad | 杨学明.1997.安徽铜陵老鸦岭层状铜矿床的成矿地球化学研究.大地構造與成矿學21(4): 347-361 | |
| AC-21 | feldspar | Baimangshanyanti | Anhui | Lower Yangtze | Polymetallic | 18.3500 | 15.6000 | 38.4600 | Bad | 邢凤鸣.1996.铜陵地区高钾钙碱系列侵入岩.地球化學25(1): 29-38 |
| AC-148 | feldspar | Yueshan | Anhui | Lower Yangtze | Polymetallic | 17.8460 | 15.4840 | 37.8110 | Bad | 邢凤鸣.1996.铜陵地区高钾钙碱系列侵入岩.地球化學25(1): 29-38 |
| feldspar | Bajiatan | Anhui | Lower Yangtze | 18.1510 | 15.5590 | 38.1940 | Bad | 黃斌1991.節錄於李文达等1998.中国东南部中生代火成岩与矿床 | ||
| feldspar | Bajiatan | Anhui | Lower Yangtze | 18.0200 | 15.5290 | 38.0700 | Bad | 黃斌1991.節錄於李文达等1998.中国东南部中生代火成岩与矿床 | ||
| feldspar | Yueshan | Anhui | Lower Yangtze | 17.8130 | 15.5200 | 38.0740 | Bad | 黃斌1991.節錄於李文达等1998.中国东南部中生代火成岩与矿床 | ||
| galena | Mashan | Anhui | Lower Yangtze | Au | 18.7110 | 15.8280 | 39.1280 | Bad | 黃斌1991.節錄於李文达等1998.中国东南部中生代火成岩与矿床 | |
| galena | Mashan | Anhui | Lower Yangtze | Au | 18.7800 | 15.7400 | 39.1100 | Bad | 黃斌1991.節錄於李文达等1998.中国东南部中生代火成岩与矿床 | |
| galena | Mashan | Anhui | Lower Yangtze | Au | 18.4960 | 15.7620 | 39.9040 | Bad | 黃斌1991.節錄於李文达等1998.中国东南部中生代火成岩与矿床 | |
| galena | Mashan | Anhui | Lower Yangtze | Au | 18.5360 | 15.7000 | 39.7260 | Bad | 黃斌1991.節錄於李文达等1998.中国东南部中生代火成岩与矿床 | |
| 1 | galena | Mashan | Anhui | Lower Yangtze | Au | 18.2200 | 15.3400 | 38.4300 | Bad | 叶敬仁.1985.长江中下游铁铜多金属矿带的铅同位素研究及其大地构造与成矿学意义.大地構造與成矿學9(4): 309-322 |
| 3 | galena | Mashan | Anhui | Lower Yangtze | Au | 18.4200 | 15.7400 | 39.4800 | Bad | 叶敬仁.1985.长江中下游铁铜多金属矿带的铅同位素研究及其大地构造与成矿学意义.大地構造與成矿學9(4): 309-322 |
| BN462 | galena | Jinlang | Anhui | Lower Yangtze | Fe | 18.2890 | 15.5430 | 38.3299 | Bad | 叶敬仁.1985.长江中下游铁铜多金属矿带的铅同位素研究及其大地构造与成矿学意义.大地構造與成矿學9(4): 309-322 |
| 85 | feldspar | Fenhuangshan | Anhui | Lower Yangtze | Polymetallic | 18.6830 | 15.5780 | 38.7760 | Bad | Li et al. 1996. Reported by Pan & Dong.1999. The Lower Changjiang metallogenic belt. Ore Geology Reviews 15: 177-242 |
| 86 | feldspar | Fenhuangshan | Anhui | Lower Yangtze | Polymetallic | 18.8490 | 15.6060 | 38.7270 | Bad | Li et al. 1996. Reported by Pan & Dong.1999. The Lower Changjiang metallogenic belt. Ore Geology Reviews 15: 177-242 |
| 97 (M681) | galena | Mashan | Anhui | Lower Yangtze | Au | 18.2940 | 15.5340 | 38.2300 | Bad | Gu.1984.Reported by Pan & Dong.1999. The Lower Changjiang metallogenic belt. Ore Geology Reviews 15: 177-242 |
| 98 (M504) | galena | Mashan | Anhui | Lower Yangtze | Au | 18.2040 | 15.5300 | 38.2050 | Bad | Gu.1984.Reported by Pan & Dong.1999. The Lower Changjiang metallogenic belt. Ore Geology Reviews 15: 177-242 |
| 103 (M676) | galena | Mashan | Anhui | Lower Yangtze | Au | 18.2730 | 15.5540 | 38.2730 | Bad | Gu.1984.Reported by Pan & Dong.1999. The Lower Changjiang metallogenic belt. Ore Geology Reviews 15: 177-242 |
| 104 (M726) | galena | Mashan | Anhui | Lower Yangtze | Au | 18.4710 | 15.5420 | 38.1930 | Bad | Gu.1984.Reported by Pan & Dong.1999. The Lower Changjiang metallogenic belt. Ore Geology Reviews 15: 177-242 |
| 105 (M625) | galena | Mashan | Anhui | Lower Yangtze | Au | 18.4750 | 15.5540 | 38.2320 | Bad | Gu.1984.Reported by Pan & Dong.1999. The Lower Changjiang metallogenic belt. Ore Geology Reviews 15: 177-242 |
| 106 (M486) | galena | Mashan | Anhui | Lower Yangtze | Au | 18.0330 | 15.5020 | 38.1390 | Bad | Gu.1984.Reported by Pan & Dong.1999. The Lower Changjiang metallogenic belt. Ore Geology Reviews 15: 177-242 |
| 107 (M630) | galena | Mashan | Anhui | Lower Yangtze | Au | 18.3370 | 15.6650 | 38.5280 | Bad | Gu.1984.Reported by Pan & Dong.1999. The Lower Changjiang metallogenic belt. Ore Geology Reviews 15: 177-242 |
| 146 | feldspar | Shizishan | Anhui | Lower Yangtze | Polymetallic | 18.2190 | 15.5500 | 38.3460 | Bad | Gu.1984.Reported by Pan & Dong.1999. The Lower Changjiang metallogenic belt. Ore Geology Reviews 15: 177-242 |
| feldspar | Tonglüshan | Hubei | Lower Yangtze | Cu-Fe | 18.1090 | 15.5340 | 38.3530 | Bad | 舒全安.1992. 鄂东铁铜矿产地质 | |
| galena | Jilongshanjin | Hubei | Lower Yangtze | Cu-Au | 18.1000 | 15.5000 | 38.2700 | Bad | 伍超群.1992.節錄於贾宝剑.2012.湖北鸡笼山矽卡岩型金铜矿床铅同位素地球化学研究.現代地質26(3): 471-477, 488 | |
| galena | Jilongshanjin | Hubei | Lower Yangtze | Cu-Au | 17.8360 | 15.5450 | 38.2440 | Bad | 舒全安.1992.節錄於贾宝剑.2012.湖北鸡笼山矽卡岩型金铜矿床铅同位素地球化学研究.現代地質26(3): 471-477, 488 | |
| feldspar | Tieshan | Hubei | Lower Yangtze | 17.8660 | 15.4530 | 37.9980 | Bad | 舒全安.1992.節錄於李文达等1998.中国东南部中生代火成岩与矿床 | ||
| feldspar | Tongshankou | Hubei | Lower Yangtze | 18.1050 | 15.5340 | 38.3530 | Bad | 舒全安.1992.節錄於李文达等1998.中国东南部中生代火成岩与矿床 | ||
| feldspar | Tonglüshan | Hubei | Lower Yangtze | Cu-Fe | 18.0470 | 15.5170 | 38.3810 | Bad | 舒全安.1992.節錄於李文达等1998.中国东南部中生代火成岩与矿床 | |
| feldspar | Chengchao | Hubei | Lower Yangtze | 18.1230 | 15.5060 | 38.4080 | Bad | 舒全安.1992.節錄於李文达等1998.中国东南部中生代火成岩与矿床 | ||
| D1 | galena | Huangshi—Guangji | Hubei | Lower Yangtze | Pb-Zn | 18.0930 | 15.5250 | 38.1730 | Bad | 周得科.1988.论黄石—广济地区下三叠统铅锌矿成矿机制及矿床成因.湖北地質2(1): 12-26 |
| D2 | galena | Huangshi—Guangji | Hubei | Lower Yangtze | Pb-Zn | 18.0810 | 15.5190 | 38.1680 | Bad | 周得科.1988.论黄石—广济地区下三叠统铅锌矿成矿机制及矿床成因.湖北地質2(1): 12-26 |
| D3 | galena | Huangshi—Guangji | Hubei | Lower Yangtze | Pb-Zn | 18.1070 | 15.5140 | 38.1760 | Bad | 周得科.1988.论黄石—广济地区下三叠统铅锌矿成矿机制及矿床成因.湖北地質2(1): 12-26 |
| &3 | galena | Huangshi—Guangji | Hubei | Lower Yangtze | Pb-Zn | 18.1400 | 15.5190 | 38.2320 | Bad | 周得科.1988.论黄石—广济地区下三叠统铅锌矿成矿机制及矿床成因.湖北地質2(1): 12-26 |
| &2-2 | galena | Huangshi—Guangji | Hubei | Lower Yangtze | Pb-Zn | 17.9970 | 15.5170 | 38.2630 | Bad | 周得科.1988.论黄石—广济地区下三叠统铅锌矿成矿机制及矿床成因.湖北地質2(1): 12-26 |
| 5e | galena | Huangshi—Guangji | Hubei | Lower Yangtze | Pb-Zn | 18.1120 | 15.4820 | 38.0450 | Bad | 周得科.1988.论黄石—广济地区下三叠统铅锌矿成矿机制及矿床成因.湖北地質2(1): 12-26 |
| 区T2 | galena | Huangshi—Guangji | Hubei | Lower Yangtze | Pb-Zn | 18.1090 | 15.4780 | 38.0550 | Bad | 周得科.1988.论黄石—广济地区下三叠统铅锌矿成矿机制及矿床成因.湖北地質2(1): 12-26 |
| 区T7 | galena | Huangshi—Guangji | Hubei | Lower Yangtze | Pb-Zn | 18.0950 | 15.5360 | 38.2210 | Bad | 周得科.1988.论黄石—广济地区下三叠统铅锌矿成矿机制及矿床成因.湖北地質2(1): 12-26 |
| 区T25-1 | galena | Huangshi—Guangji | Hubei | Lower Yangtze | Pb-Zn | 17.7000 | 15.4630 | 37.9700 | Bad | 周得科.1988.论黄石—广济地区下三叠统铅锌矿成矿机制及矿床成因.湖北地質2(1): 12-26 |
| B8-1 | galena | Huangshi—Guangji | Hubei | Lower Yangtze | Pb-Zn | 17.9320 | 15.4370 | 38.0150 | Bad | 周得科.1988.论黄石—广济地区下三叠统铅锌矿成矿机制及矿床成因.湖北地質2(1): 12-26 |
| B8-2 | galena | Huangshi—Guangji | Hubei | Lower Yangtze | Pb-Zn | 18.0050 | 15.4270 | 38.1900 | Bad | 周得科.1988.论黄石—广济地区下三叠统铅锌矿成矿机制及矿床成因.湖北地質2(1): 12-26 |
| k5 | galena | Huangshi—Guangji | Hubei | Lower Yangtze | Pb-Zn | 18.0530 | 15.5790 | 38.3390 | Bad | 周得科.1988.论黄石—广济地区下三叠统铅锌矿成矿机制及矿床成因.湖北地質2(1): 12-26 |
| feldspar | Malong | Hubei | Lower Yangtze | 17.3900 | 15.4820 | 37.7140 | Bad | 王彤.1990.湖北桐柏——大别地区花岗岩的长石铅同位素组成特征及其地质意义.湖北地質2: 27-39 |