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Rhodochrosite from
Yonaguni Knoll IV Hydrothermal Field, Okinawa Trough, Senkaku Islands (Diaoyudao Islands; Diaoyutai Islands), Ishigaki City, Okinawa Prefecture, Japan


Locality type:Hydrothermal Vent
Classification
Species:Rhodochrosite
Formula:MnCO3
Confirmation
Validity:Believed Valid
Data
Mineral Data:Click here to view Rhodochrosite 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
Mindat Occurrence Record ID:898212
Long-form Identifier:1:3:898212:4
GUID (UUID V4):1cd2549c-f350-443a-ab13-a970bbedf8de
Nearest other occurrences of Rhodochrosite
85.3km (53.0 miles) Jiufen Mine (Chiufen Mine), Jui-Fang Town, Gongliao 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
Reference Search (possible matching items)
Journal (article/letter/editorial)
Sulfide Chimney, Yonaguni Knoll IV Hydrothermal Field, Southern Okinawa Trough, Japan: The First Reported...Sn-Bearing Chalcopyrite in an Active Seafloor Hydrothermal System Kaul Gena,1 Hitoshi Chiba,2 Katsuo Kase...and Resource Science, Akita University, Akita, Japan Abstract A sulfide chimney ore sampled from the...Tiger vent area in the Yonaguni Knoll IV hydrothermal field, south Okinawa trough, consists of anhydrite...occurrence of such minerals in an active submarine hydrothermal system. The results confirm that Sn enters the
Journal (article/letter/editorial)
Separation of Hydrothermal Fluid: Case Study of the Yonaguni Knoll IV Hydrothermal Field in the Okinawa Trough...Faculty of Sciences, Kyushu University, Fukuoka, Japan, 2Department of Earth and Planetary System Science...Faculty of Science, Hokkaido University, Sapporo, Japan, and 3Department of Earth Sciences, Faculty of Science...University, Okayama, Japan Abstract The Yonaguni Knoll IV hydrothermal vent field (24°51′N, 122°42′E)...1370–1385 m near the western edge of the southern Okinawa Trough. During the YK03–05 and YK04–05 expeditions
Book
Processes 3.5 The SCS and Okinawa Trough 3.5.1 SCS basin 3.5.2 Okinawa Trough 3.6 Magmatisms and Neotectonics... vi Contents 3.6.3 Regional Seismicity 3.6.4 Hydrothermal Activities 3.6.5 Post-Miocene Continental Margin...Organic Carbon 4.6 Volcanic Sediments 4.6.1 Okinawa Trough Volcanic Deposition 4.6.2 South China Sea Volcanic...Paleoceanography: Long-Term Trends 6.2.1 East China Sea: Okinawa Trough 6.2.2 South China Sea: Ocean Connection and...the successive discoveries of gas hydrates and hydrothermal vents have also stimulated geological investigations
 
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