| Locality type: | Hydrothermal Vent |
| Classification |
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| Species: | Pyrite |
| Formula: | FeS2 |
| Confirmation |
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| Validity: | Believed Valid |
| Data |
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| Mineral Data: | Click here to view Pyrite data |
| Locality Data: | Click here to view Yonaguni Knoll IV Hydrothermal Field, Okinawa Trough, Senkaku Islands (Diaoyudao Islands; Diaoyutai Islands), Ishigaki City, Okinawa Prefecture, Japan |
| Data Identifiers |
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| Mindat Occurrence Record ID: | 898221 |
| Long-form Identifier: | 1:3:898221:6 |
| GUID (UUID V4): | 0 |
| Localities for Pyrite in this Region |
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| Tiger Sulfide Chimney, Yonaguni Knoll IV Hydrothermal Field, Okinawa Trough, Senkaku Islands (Diaoyudao Islands; Diaoyutai Islands), Ishigaki City, Okinawa Prefecture, Japan |
| Nearest other occurrences of Pyrite |
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| 0.3km (0.2 miles) | ⓘTiger Sulfide Chimney, Yonaguni Knoll IV Hydrothermal Field, Okinawa Trough, Senkaku Islands (Diaoyudao Islands; Diaoyutai Islands), Ishigaki City, Okinawa Prefecture, Japan |
| 78.1km (48.5 miles) | ⓘLailai Dike, Toucheng Township, Yilan County, Taiwan |
| 88.7km (55.1 miles) | ⓘPinglin deposit, Hsinliaotze, Shuangxi District, New Taipei City, Taiwan |
| 88.8km (55.2 miles) | ⓘHsumei orebody, Ruifang District, New Taipei City, Taiwan |
| 88.9km (55.2 miles) | ⓘThird Changjen Orebody (3rd Changjen), Chinkuashih mine, Ruifang District, New Taipei City, Taiwan |
| 89.3km (55.5 miles) | ⓘPenshan Orebody (Penshan Vein; The Main Vein), Chinkuashih mine, Ruifang District, New Taipei City, Taiwan |
| 89.4km (55.6 miles) | ⓘFirst Changjen Orebody (1st Changjen), Chinkuashih mine, Ruifang District, New Taipei City, Taiwan |
| 90.1km (56.0 miles) | ⓘFu-Shan Gold Mine, Ruifang District, New Taipei City, Taiwan |
| 90.5km (56.2 miles) | ⓘJiufen Mine (Chiufen Mine), Ruifang District, New Taipei City, Taiwan |
| 90.7km (56.3 miles) | ⓘChinkuashih mine, Ruifang District, New Taipei City, Taiwan |
| References |
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Suzuki, R., Ishibashi, J. I., Nakaseama, M., Konno, U., Tsunogai, U., Gena, K., & Chiba, H. (2008). Diverse range of mineralization induced by phase separation of hydrothermal fluid: Case study of the Yonaguni Knoll IV Hydrothermal Field in the Okinawa Trough Back‐Arc Basin. Resource geology, 58(3), 267-288. |
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