Locality type: | Hydrothermal Vent |
Classification |
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Species: | 'Tetrahedrite Subgroup' (not an IMA approved species) |
Formula: | Cu6(Cu4C22+)Sb4S12S |
Confirmation |
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Validity: | Believed Valid |
Data |
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Mineral Data: | Click here to view Tetrahedrite Subgroup 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: | 898209 |
Long-form Identifier: | 1:3:898209:4 |
GUID (UUID V4): | fa3ce36f-3acb-4f78-8608-869e00f20757 |
Nearest other occurrences of Tetrahedrite Subgroup |
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85.3km (53.0 miles) | ⓘJiufen Mine (Chiufen Mine), Jui-Fang Town, Gongliao 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 |
90.1km (56.0 miles) | ⓘFu-Shan Gold 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. |