Hsu & Sabatini (2019) — 5,886 geological ore samples
5886 samples found (page 35/118)
| Sample No. | Specimen | Site (English) | Admin Province | Metal Province | Metal Type | ²⁰⁶Pb/²⁰⁴Pb | ²⁰⁷Pb/²⁰⁴Pb | ²⁰⁸Pb/²⁰⁴Pb | Quality | Reference |
|---|---|---|---|---|---|---|---|---|---|---|
| galena | Chengchong | Hunan | Lower Yangtze | Polymetallic | 18.4300 | 15.7190 | 38.8390 | Good | 刘女后群.2001.湘东北斑岩型和热液脉型铜矿成矿物质来源探讨.華南地質與礦產1: 41-47 | |
| galena | Qibaoshan | Hunan | Lower Yangtze | Polymetallic | 18.2870 | 15.5960 | 38.4640 | Good | 刘女后群.2001.湘东北斑岩型和热液脉型铜矿成矿物质来源探讨.華南地質與礦產1: 41-47 | |
| galena | Qibaoshan | Hunan | Lower Yangtze | Polymetallic | 18.3130 | 15.6810 | 38.7460 | Good | 刘女后群.2001.湘东北斑岩型和热液脉型铜矿成矿物质来源探讨.華南地質與礦產1: 41-47 | |
| galena | Qibaoshan | Hunan | Lower Yangtze | Polymetallic | 18.1180 | 15.5370 | 38.8820 | Good | 刘女后群.2001.湘东北斑岩型和热液脉型铜矿成矿物质来源探讨.華南地質與礦產1: 41-47 | |
| galena | Qibaoshan | Hunan | Lower Yangtze | Polymetallic | 18.4780 | 15.6280 | 38.7080 | Good | 刘女后群.2001.湘东北斑岩型和热液脉型铜矿成矿物质来源探讨.華南地質與礦產1: 41-47 | |
| galena | Qibaoshan | Hunan | Lower Yangtze | Polymetallic | 18.4670 | 15.6630 | 38.8060 | Good | 刘女后群.2001.湘东北斑岩型和热液脉型铜矿成矿物质来源探讨.華南地質與礦產1: 41-47 | |
| galena | Qibaoshan | Hunan | Lower Yangtze | Polymetallic | 18.4200 | 15.7230 | 38.8180 | Good | 刘女后群.2001.湘东北斑岩型和热液脉型铜矿成矿物质来源探讨.華南地質與礦產1: 41-47 | |
| galena | Qibaoshan | Hunan | Lower Yangtze | Polymetallic | 18.2680 | 15.6020 | 38.4680 | Good | 刘女后群.2001.湘东北斑岩型和热液脉型铜矿成矿物质来源探讨.華南地質與礦產1: 41-47 | |
| galena | Qibaoshan | Hunan | Lower Yangtze | Polymetallic | 18.1000 | 15.6260 | 38.6280 | Good | 刘女后群.2001.湘东北斑岩型和热液脉型铜矿成矿物质来源探讨.華南地質與礦產1: 41-47 | |
| galena | Qibaoshan | Hunan | Lower Yangtze | Polymetallic | 18.3720 | 15.8090 | 38.9480 | Good | 刘女后群.2001.湘东北斑岩型和热液脉型铜矿成矿物质来源探讨.華南地質與礦產1: 41-47 | |
| TS-1 | galena | Tongcun | Zhejiang | Lower Yangtze | Cu-Mo | 18.3140 | 15.6460 | 38.7840 | Good | 朱玉娣.2014.浙西桐村斑岩钼铜矿含矿花岗岩成岩成矿作用.中國地質大學博士論文 |
| TS-4 | galena | Tongcun | Zhejiang | Lower Yangtze | Cu-Mo | 18.3140 | 15.6480 | 38.7900 | Good | 朱玉娣.2014.浙西桐村斑岩钼铜矿含矿花岗岩成岩成矿作用.中國地質大學博士論文 |
| TS-8 | galena | Tongcun | Zhejiang | Lower Yangtze | Cu-Mo | 18.3440 | 15.6760 | 38.8750 | Good | 朱玉娣.2014.浙西桐村斑岩钼铜矿含矿花岗岩成岩成矿作用.中國地質大學博士論文 |
| TS-9 | galena | Tongcun | Zhejiang | Lower Yangtze | Cu-Mo | 18.3150 | 15.6430 | 38.7690 | Good | 朱玉娣.2014.浙西桐村斑岩钼铜矿含矿花岗岩成岩成矿作用.中國地質大學博士論文 |
| LG-501 | feldspar | Kaihuashiershan | Zhejiang | Lower Yangtze | 18.0740 | 15.5930 | 38.0280 | Good | 王一先.1997.浙江花岗岩类地球化学与地壳演化──Ⅰ.显生宙花岗岩类.地球化學26(6): 57-68 | |
| LG-83 | feldspar | Fuyan | Zhejiang | Lower Yangtze | 17.8600 | 15.4030 | 37.5000 | Good | 王一先.1997.浙江花岗岩类地球化学与地壳演化──Ⅰ.显生宙花岗岩类.地球化學26(6): 57-68 | |
| 3 | galena | Jiande | Zhejiang | Lower Yangtze | Polymetallic | 18.0910 | 15.6530 | 38.3410 | Bad | 刘家军.1997.浙江建德块状硫化物矿床地球化学特征及其成因意义.地質地球化學2: 31-35 |
| 4 | galena | Jiande | Zhejiang | Lower Yangtze | Polymetallic | 17.9710 | 15.5600 | 38.0720 | Bad | 刘家军.1997.浙江建德块状硫化物矿床地球化学特征及其成因意义.地質地球化學2: 31-35 |
| 5 | galena | Jiande | Zhejiang | Lower Yangtze | Polymetallic | 18.0010 | 15.5490 | 37.9760 | Bad | 徐跃通等1993.節錄於刘家军.1997.浙江建德块状硫化物矿床地球化学特征及其成因意义.地質地球化學2: 31-35 |
| 6 | galena | Jiande | Zhejiang | Lower Yangtze | Polymetallic | 18.1100 | 15.6610 | 38.3310 | Bad | 徐跃通等1993.節錄於刘家军.1997.浙江建德块状硫化物矿床地球化学特征及其成因意义.地質地球化學2: 31-35 |
| 7 | galena | Jiande | Zhejiang | Lower Yangtze | Polymetallic | 18.0780 | 15.6270 | 38.1900 | Bad | 徐跃通等1993.節錄於刘家军.1997.浙江建德块状硫化物矿床地球化学特征及其成因意义.地質地球化學2: 31-35 |
| 8 | galena | Jiande | Zhejiang | Lower Yangtze | Polymetallic | 18.0770 | 15.5830 | 38.2790 | Bad | 徐跃通等1993.節錄於刘家军.1997.浙江建德块状硫化物矿床地球化学特征及其成因意义.地質地球化學2: 31-35 |
| 9 | galena | Jiande | Zhejiang | Lower Yangtze | Polymetallic | 17.9580 | 15.5730 | 38.1160 | Bad | 徐跃通等1993.節錄於刘家军.1997.浙江建德块状硫化物矿床地球化学特征及其成因意义.地質地球化學2: 31-35 |
| GK205 | galena | Anji | Zhejiang | Lower Yangtze | Polymetallic | 18.3910 | 15.6050 | 38.4200 | Good | 李应栩.2012.浙江安吉港口多金属矿床铅物质来源初探——铅同位素证据.矿床與地質31(4): 917-929 |
| GK209 | galena | Anji | Zhejiang | Lower Yangtze | Polymetallic | 18.4080 | 15.6210 | 38.4610 | Good | 李应栩.2012.浙江安吉港口多金属矿床铅物质来源初探——铅同位素证据.矿床與地質31(4): 917-929 |
| GK211 | galena | Anji | Zhejiang | Lower Yangtze | Polymetallic | 18.3840 | 15.6130 | 38.4590 | Good | 李应栩.2012.浙江安吉港口多金属矿床铅物质来源初探——铅同位素证据.矿床與地質31(4): 917-929 |
| GK212 | galena | Anji | Zhejiang | Lower Yangtze | Polymetallic | 18.3310 | 15.6100 | 38.4590 | Good | 李应栩.2012.浙江安吉港口多金属矿床铅物质来源初探——铅同位素证据.矿床與地質31(4): 917-929 |
| GK213 | galena | Anji | Zhejiang | Lower Yangtze | Polymetallic | 18.4000 | 15.5820 | 38.3280 | Good | 李应栩.2012.浙江安吉港口多金属矿床铅物质来源初探——铅同位素证据.矿床與地質31(4): 917-929 |
| GK215 | galena | Anji | Zhejiang | Lower Yangtze | Polymetallic | 18.3910 | 15.6000 | 38.3970 | Good | 李应栩.2012.浙江安吉港口多金属矿床铅物质来源初探——铅同位素证据.矿床與地質31(4): 917-929 |
| GK228 | galena | Anji | Zhejiang | Lower Yangtze | Polymetallic | 18.3640 | 15.6070 | 38.4260 | Good | 李应栩.2012.浙江安吉港口多金属矿床铅物质来源初探——铅同位素证据.矿床與地質31(4): 917-929 |
| GK229 | galena | Anji | Zhejiang | Lower Yangtze | Polymetallic | 18.3740 | 15.5880 | 38.3620 | Good | 李应栩.2012.浙江安吉港口多金属矿床铅物质来源初探——铅同位素证据.矿床與地質31(4): 917-929 |
| GK230 | galena | Anji | Zhejiang | Lower Yangtze | Polymetallic | 18.5660 | 15.6400 | 38.5010 | Good | 李应栩.2012.浙江安吉港口多金属矿床铅物质来源初探——铅同位素证据.矿床與地質31(4): 917-929 |
| YJ-01 | galena | Anji | Zhejiang | Lower Yangtze | Polymetallic | 18.3670 | 15.6030 | 38.4350 | Good | 李应栩.2012.浙江安吉港口多金属矿床铅物质来源初探——铅同位素证据.矿床與地質31(4): 917-929 |
| L-19 | galena | Ningwu | Jiangsu | Lower Yangtze | Fe | 18.2000 | 15.4500 | 38.4200 | 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 |
| L-28 | galena | Ningwu | Jiangsu | Lower Yangtze | Fe | 18.1500 | 15.5700 | 38.2300 | 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 |
| J.-21 | galena | Ningwu | Jiangsu | Lower Yangtze | Fe | 18.3700 | 15.5400 | 38.6400 | 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 |
| L-22 | galena | Ningwu | Jiangsu | Lower Yangtze | Fe | 18.6100 | 15.4600 | 38.7600 | 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 |
| feldspar | Suzhou | Jiangsu | Lower Yangtze | 17.3940 | 15.4270 | 37.8000 | Bad | 張理剛1994,盧志良1988.節錄於李文达等1998.中国东南部中生代火成岩与矿床 | ||
| feldspar | Suzhou | Jiangsu | Lower Yangtze | 17.4470 | 15.4170 | 37.7950 | Bad | 張理剛1994,盧志良1988.節錄於李文达等1998.中国东南部中生代火成岩与矿床 | ||
| feldspar | Suzhou | Jiangsu | Lower Yangtze | 17.3770 | 15.4090 | 37.7160 | Bad | 張理剛1994,盧志良1988.節錄於李文达等1998.中国东南部中生代火成岩与矿床 | ||
| feldspar | Suzhou | Jiangsu | Lower Yangtze | 17.5120 | 15.3920 | 37.6620 | Bad | 張理剛1994,盧志良1988.節錄於李文达等1998.中国东南部中生代火成岩与矿床 | ||
| feldspar | Suzhou | Jiangsu | Lower Yangtze | 17.0620 | 15.3020 | 37.4420 | Bad | 張理剛1994,盧志良1988.節錄於李文达等1998.中国东南部中生代火成岩与矿床 | ||
| feldspar | Suzhou | Jiangsu | Lower Yangtze | 17.1330 | 15.3120 | 37.5030 | Bad | 張理剛1994,盧志良1988.節錄於李文达等1998.中国东南部中生代火成岩与矿床 | ||
| feldspar | Suzhou | Jiangsu | Lower Yangtze | 17.3870 | 15.3700 | 37.9800 | Bad | 張理剛1994,盧志良1988.節錄於李文达等1998.中国东南部中生代火成岩与矿床 | ||
| feldspar | Zhongjiu | Anhui | Lower Yangtze | 18.2680 | 15.5900 | 38.2640 | Bad | 邢鳳鳴1995.節錄於李文达等1998.中国东南部中生代火成岩与矿床 | ||
| feldspar | Aoshan | Anhui | Lower Yangtze | 18.3750 | 15.5890 | 38.3710 | Bad | 邢鳳鳴1995.節錄於李文达等1998.中国东南部中生代火成岩与矿床 | ||
| feldspar | Taocun | Jiangsu | Lower Yangtze | 18.3350 | 15.6300 | 38.5430 | Bad | 邢鳳鳴1995.節錄於李文达等1998.中国东南部中生代火成岩与矿床 | ||
| feldspar | Yanghutang | Anhui | Lower Yangtze | 18.0730 | 15.4730 | 37.9510 | Bad | 邢鳳鳴1995.節錄於李文达等1998.中国东南部中生代火成岩与矿床 | ||
| feldspar | Gushan | Anhui | Lower Yangtze | 18.8300 | 15.7400 | 38.8700 | Bad | 邢鳳鳴1995.節錄於李文达等1998.中国东南部中生代火成岩与矿床 | ||
| feldspar | Huoli | Anhui | Lower Yangtze | 18.3880 | 15.5200 | 38.2700 | Bad | 邢鳳鳴1995.節錄於李文达等1998.中国东南部中生代火成岩与矿床 |