Hsu & Sabatini (2019) — 5,886 geological ore samples
5886 samples found (page 1/118)
| Sample No. | Specimen | Site (English) | Admin Province | Metal Province | Metal Type | ²⁰⁶Pb/²⁰⁴Pb | ²⁰⁷Pb/²⁰⁴Pb | ²⁰⁸Pb/²⁰⁴Pb | Quality | Reference |
|---|---|---|---|---|---|---|---|---|---|---|
| K10—TC2 | galena | Ashelei | Xinjiang | Altai-Junggel | Cu | 17.9330 | 15.6380 | 38.4130 | Bad | 王登紅.1996.新疆阿舍勒火山岩型块状硫化物铜矿硫、铅同位素地球化学. 地球化學25(6): 582-590 |
| 89K10—3 | galena | Ashelei | Xinjiang | Altai-Junggel | Cu | 17.8850 | 15.5100 | 37.7270 | Bad | 王登紅.1996.新疆阿舍勒火山岩型块状硫化物铜矿硫、铅同位素地球化学. 地球化學25(6): 582-590 |
| 89K10—3—2 | galena | Ashelei | Xinjiang | Altai-Junggel | Cu | 19.9390 | 15.5840 | 37.9800 | Bad | 王登紅.1996.新疆阿舍勒火山岩型块状硫化物铜矿硫、铅同位素地球化学. 地球化學25(6): 582-590 |
| QK10 | feldspar | South altai | Xinjiang | Altai-Junggel | 18.3240 | 15.5090 | 38.6410 | Bad | 曲国胜.1991.阿尔泰造山带的铅同位素地质及其构造意义.現代地質5(1): 100-110 | |
| ALT17-1 | feldspar | South altai | Xinjiang | Altai-Junggel | 18.2370 | 15.5510 | 38.1740 | Bad | 曲国胜.1991.阿尔泰造山带的铅同位素地质及其构造意义.現代地質5(1): 100-110 | |
| ALT13-1 | feldspar | South altai | Xinjiang | Altai-Junggel | 18.5090 | 15.5790 | 38.1450 | Bad | 曲国胜.1991.阿尔泰造山带的铅同位素地质及其构造意义.現代地質5(1): 100-110 | |
| WQK2-11 | feldspar | South altai | Xinjiang | Altai-Junggel | 18.3600 | 15.5830 | 38.3230 | Bad | 曲国胜.1991.阿尔泰造山带的铅同位素地质及其构造意义.現代地質5(1): 100-110 | |
| HZ2-1 | feldspar | South altai | Xinjiang | Altai-Junggel | 18.6390 | 15.6870 | 38.5280 | Bad | 曲国胜.1991.阿尔泰造山带的铅同位素地质及其构造意义.現代地質5(1): 100-110 | |
| KKT3-1 | feldspar | South altai | Xinjiang | Altai-Junggel | 18.4990 | 15.6040 | 38.0950 | Bad | 曲国胜.1991.阿尔泰造山带的铅同位素地质及其构造意义.現代地質5(1): 100-110 | |
| QH1-14 | feldspar | South altai | Xinjiang | Altai-Junggel | 18.3120 | 15.5880 | 38.2790 | Bad | 曲国胜.1991.阿尔泰造山带的铅同位素地质及其构造意义.現代地質5(1): 100-110 | |
| QK31 | feldspar | Qiongkuer-Abagong | Xinjiang | Altai-Junggel | 18.3330 | 15.5980 | 38.1060 | Bad | 曲国胜.1991.阿尔泰造山带的铅同位素地质及其构造意义.現代地質5(1): 100-110 | |
| ALT7-17 | feldspar | Qiongkuer-abagong | Xinjiang | Altai-Junggel | 18.6660 | 15.5950 | 38.3660 | Bad | 曲国胜.1991.阿尔泰造山带的铅同位素地质及其构造意义.現代地質5(1): 100-110 | |
| FY12-1 | feldspar | Qiongkuer-abagong | Xinjiang | Altai-Junggel | 18.4090 | 15.7340 | 38.5650 | Bad | 曲国胜.1991.阿尔泰造山带的铅同位素地质及其构造意义.現代地質5(1): 100-110 | |
| CH9-6 | feldspar | Qiongkuer-abagong | Xinjiang | Altai-Junggel | 18.5210 | 15.7480 | 38.5820 | Bad | 曲国胜.1991.阿尔泰造山带的铅同位素地质及其构造意义.現代地質5(1): 100-110 | |
| CH4-4 | feldspar | Qiongkuer-abagong | Xinjiang | Altai-Junggel | 18.5490 | 15.6690 | 38.3100 | Bad | 曲国胜.1991.阿尔泰造山带的铅同位素地质及其构造意义.現代地質5(1): 100-110 | |
| FWX1-1 | feldspar | Eerjisi | Xinjiang | Altai-Junggel | 17.9730 | 15.4220 | 38.9200 | Bad | 曲国胜.1991.阿尔泰造山带的铅同位素地质及其构造意义.現代地質5(1): 100-110 | |
| FY4-8 | feldspar | Eerjisi | Xinjiang | Altai-Junggel | 19.5810 | 15.6380 | 38.7000 | Bad | 曲国胜.1991.阿尔泰造山带的铅同位素地质及其构造意义.現代地質5(1): 100-110 | |
| FY7-31 | feldspar | Eerjisi | Xinjiang | Altai-Junggel | 18.2010 | 15.4810 | 37.7800 | Bad | 曲国胜.1991.阿尔泰造山带的铅同位素地质及其构造意义.現代地質5(1): 100-110 | |
| AL5-2 | feldspar | Eerjisi | Xinjiang | Altai-Junggel | 18.3780 | 15.6180 | 38.2070 | Bad | 曲国胜.1991.阿尔泰造山带的铅同位素地质及其构造意义.現代地質5(1): 100-110 | |
| ET9-1 | feldspar | Buerjin-ertai | Xinjiang | Altai-Junggel | 18.3980 | 15.5030 | 38.2030 | Bad | 曲国胜.1991.阿尔泰造山带的铅同位素地质及其构造意义.現代地質5(1): 100-110 | |
| HATD-6 | feldspar | Aketishenkan | Xinjiang | Altai-Junggel | Au | 18.6900 | 15.5220 | 38.0470 | Good | 袁峰.2001.新疆阿克提什坎金矿床铅同位素地球化学.合肥工業大學學報24(1): 12-16 |
| HAT-04 | galena | Aketishenkan | Xinjiang | Altai-Junggel | Au | 18.3530 | 15.5290 | 38.1380 | Good | 袁峰.2001.新疆阿克提什坎金矿床铅同位素地球化学.合肥工業大學學報24(1): 12-16 |
| T87080 | galena | Tiemuerte | Xinjiang | Altai-Junggel | Cu-Pb-Zn | 18.1010 | 15.4800 | 37.7770 | Good | 姜俊.2003.鐵米木爾特多金屬礦床地質特徵及成因探討.新疆有色金屬2:2-5 |
| T88455 | galena | Tiemuerte | Xinjiang | Altai-Junggel | Cu-Pb-Zn | 17.9590 | 15.4960 | 37.6100 | Good | 姜俊.2003.鐵米木爾特多金屬礦床地質特徵及成因探討.新疆有色金屬2:2-5 |
| 161/1 | feldspar | Taerlang | Xinjiang | Altai-Junggel | 18.2450 | 15.4990 | 38.0270 | Good | 童英.2006.中国阿尔泰造山带花岗岩Pb同位素组成特征：幔源成因佐证及陆売生长意义.地質學報80(4): 517-528 | |
| 164 | feldspar | Taerlang | Xinjiang | Altai-Junggel | 18.1950 | 15.5180 | 37.9510 | Good | 童英.2006.中国阿尔泰造山带花岗岩Pb同位素组成特征：幔源成因佐证及陆売生长意义.地質學報80(4): 517-528 | |
| 165 | feldspar | Taerlang | Xinjiang | Altai-Junggel | 18.1590 | 15.5060 | 37.8460 | Good | 童英.2006.中国阿尔泰造山带花岗岩Pb同位素组成特征：幔源成因佐证及陆売生长意义.地質學報80(4): 517-528 | |
| 168 | feldspar | Taerlang | Xinjiang | Altai-Junggel | 18.1160 | 15.5380 | 37.9340 | Good | 童英.2006.中国阿尔泰造山带花岗岩Pb同位素组成特征：幔源成因佐证及陆売生长意义.地質學報80(4): 517-528 | |
| 169/1 | feldspar | Taerlang | Xinjiang | Altai-Junggel | 18.2750 | 15.5690 | 38.0200 | Good | 童英.2006.中国阿尔泰造山带花岗岩Pb同位素组成特征：幔源成因佐证及陆売生长意义.地質學報80(4): 517-528 | |
| 112/2 | feldspar | Keketuohai | Xinjiang | Altai-Junggel | 18.2630 | 15.5340 | 37.9610 | Good | 童英.2006.中国阿尔泰造山带花岗岩Pb同位素组成特征：幔源成因佐证及陆売生长意义.地質學報80(4): 517-528 | |
| 116 | feldspar | Keketuohai | Xinjiang | Altai-Junggel | 18.2300 | 15.5180 | 37.8420 | Good | 童英.2006.中国阿尔泰造山带花岗岩Pb同位素组成特征：幔源成因佐证及陆売生长意义.地質學報80(4): 517-528 | |
| 106/1 | feldspar | Keketuohai | Xinjiang | Altai-Junggel | 18.0820 | 15.5080 | 37.7210 | Good | 童英.2006.中国阿尔泰造山带花岗岩Pb同位素组成特征：幔源成因佐证及陆売生长意义.地質學報80(4): 517-528 | |
| 107/1 | feldspar | Keketuohai | Xinjiang | Altai-Junggel | 18.1670 | 15.5260 | 37.8030 | Good | 童英.2006.中国阿尔泰造山带花岗岩Pb同位素组成特征：幔源成因佐证及陆売生长意义.地質學報80(4): 517-528 | |
| 120/3 | feldspar | Keketuohai | Xinjiang | Altai-Junggel | 18.3980 | 15.5580 | 38.0800 | Good | 童英.2006.中国阿尔泰造山带花岗岩Pb同位素组成特征：幔源成因佐证及陆売生长意义.地質學報80(4): 517-528 | |
| 131/1 | feldspar | Tuerhong | Xinjiang | Altai-Junggel | 18.1820 | 15.5330 | 37.8900 | Good | 童英.2006.中国阿尔泰造山带花岗岩Pb同位素组成特征：幔源成因佐证及陆売生长意义.地質學報80(4): 517-528 | |
| 132 | feldspar | Tuerhong | Xinjiang | Altai-Junggel | 18.2130 | 15.5310 | 37.8660 | Good | 童英.2006.中国阿尔泰造山带花岗岩Pb同位素组成特征：幔源成因佐证及陆売生长意义.地質學報80(4): 517-528 | |
| 138-1 | feldspar | Aweitan | Xinjiang | Altai-Junggel | 18.1480 | 15.5040 | 37.8770 | Good | 童英.2006.中国阿尔泰造山带花岗岩Pb同位素组成特征：幔源成因佐证及陆売生长意义.地質學報80(4): 517-528 | |
| 138-2 | feldspar | Aweitan | Xinjiang | Altai-Junggel | 18.1460 | 15.4960 | 37.8690 | Good | 童英.2006.中国阿尔泰造山带花岗岩Pb同位素组成特征：幔源成因佐证及陆売生长意义.地質學報80(4): 517-528 | |
| 149/3 | feldspar | Daqiao | Xinjiang | Altai-Junggel | 18.2890 | 15.5330 | 38.1870 | Good | 童英.2006.中国阿尔泰造山带花岗岩Pb同位素组成特征：幔源成因佐证及陆売生长意义.地質學報80(4): 517-528 | |
| 151 | feldspar | Daqiao | Xinjiang | Altai-Junggel | 18.3930 | 15.5470 | 38.1230 | Good | 童英.2006.中国阿尔泰造山带花岗岩Pb同位素组成特征：幔源成因佐证及陆売生长意义.地質學報80(4): 517-528 | |
| 152 | feldspar | Daqiao | Xinjiang | Altai-Junggel | 18.4220 | 15.5990 | 38.2620 | Good | 童英.2006.中国阿尔泰造山带花岗岩Pb同位素组成特征：幔源成因佐证及陆売生长意义.地質學報80(4): 517-528 | |
| 153 | feldspar | Daqiao | Xinjiang | Altai-Junggel | 18.9210 | 15.5990 | 38.1520 | Good | 童英.2006.中国阿尔泰造山带花岗岩Pb同位素组成特征：幔源成因佐证及陆売生长意义.地質學報80(4): 517-528 | |
| 157/2 | feldspar | Jiashenkalagai | Xinjiang | Altai-Junggel | 18.5400 | 15.5470 | 38.1800 | Good | 童英.2006.中国阿尔泰造山带花岗岩Pb同位素组成特征：幔源成因佐证及陆売生长意义.地質學報80(4): 517-528 | |
| 157/3 | feldspar | Jiashenkalagai | Xinjiang | Altai-Junggel | 18.4370 | 15.5320 | 38.0710 | Good | 童英.2006.中国阿尔泰造山带花岗岩Pb同位素组成特征：幔源成因佐证及陆売生长意义.地質學報80(4): 517-528 | |
| 158-1 | feldspar | Wuliqi | Xinjiang | Altai-Junggel | 18.3120 | 15.5420 | 37.9600 | Good | 童英.2006.中国阿尔泰造山带花岗岩Pb同位素组成特征：幔源成因佐证及陆売生长意义.地質學報80(4): 517-528 | |
| 256/2 | feldspar | Lamazhao | Xinjiang | Altai-Junggel | 18.3470 | 15.5290 | 37.9740 | Good | 童英.2006.中国阿尔泰造山带花岗岩Pb同位素组成特征：幔源成因佐证及陆売生长意义.地質學報80(4): 517-528 | |
| 258 | feldspar | Lamazhao | Xinjiang | Altai-Junggel | 18.3450 | 15.5530 | 38.0780 | Good | 童英.2006.中国阿尔泰造山带花岗岩Pb同位素组成特征：幔源成因佐证及陆売生长意义.地質學報80(4): 517-528 | |
| 259/1 | feldspar | Lamazhao | Xinjiang | Altai-Junggel | 18.2410 | 15.5070 | 37.9470 | Good | 童英.2006.中国阿尔泰造山带花岗岩Pb同位素组成特征：幔源成因佐证及陆売生长意义.地質學報80(4): 517-528 | |
| 141 | feldspar | Tangbahu | Xinjiang | Altai-Junggel | 18.0990 | 15.5120 | 37.7320 | Good | 童英.2006.中国阿尔泰造山带花岗岩Pb同位素组成特征：幔源成因佐证及陆売生长意义.地質學報80(4): 517-528 | |
| 186/3 | feldspar | Fuyun | Xinjiang | Altai-Junggel | 18.0600 | 15.4600 | 37.7270 | Good | 童英.2006.中国阿尔泰造山带花岗岩Pb同位素组成特征：幔源成因佐证及陆売生长意义.地質學報80(4): 517-528 |