Observation of manganese deposits on Kaikata Seamount, Izu-Ogasawara (Bonin) Arc by the Shikai 2000 submersible
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| Natura: | Dataset Open Access |
| Lingua: | en |
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PANGAEA
1992
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| _version_ | 1867169121930575872 |
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| author | Usui, Akira Nishimura, Akira |
| author_facet | Usui, Akira Nishimura, Akira |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | During Dive 408 of Shinkai 2000 on the flank of the Kaikata Seamount located on the volcanic front of the Izu-Ogasawara (Bonin) Arc, possibly recent hydrothermal manganese deposits were observed on sandy volcanic sediments at water depths of between 800 and 1200 m. The deposits cover almost the entire surface sediment across the manganese belt on the northwestern flank on the seamount on a scale of kilometers. The occurrence of the deposits, seafloor morphology and temperature of the sediments, together with previous shipboard results, lead to a possible model for the formation of the manganese deposits: A low-temperature hydrothermal solution ascends through fractures or faults in the volcanic substrate into permeable volcanic sands and precipitates manganate minerals which cement several centimeters of surface sand as hardpan. More intense and probably intermittent discharge of hydrothermal solution follows and forms many typical ridge-like vents and mounds on the seafloor. Subsequently, pure dense manganate layers developed beneath the semi-consolidated volcanic sandstone and act as a cap to the ascending fluids. The proposed mechanism may be the dominant type of low-temperature hydrothermal mineralization in submarine island-arc volcanoes and rifts. Similar hydrothermal manganese deopsits most probably occur in other active areas of the modern seafloors and in inactive island arcs. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_880486 |
| institution | PANGAEA |
| language | en |
| publishDate | 1992 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Observation of manganese deposits on Kaikata Seamount, Izu-Ogasawara (Bonin) Arc by the Shikai 2000 submersible Usui, Akira Nishimura, Akira Date/Time of event; Deposit type; DEPTH, sediment/rock; Description; DV408/St_1; DV408/St_2; DV408/St_3; DV408/St_4; Elevation of event; Event label; Kaikata Seamount, Pacific Ocean; Latitude of event; Longitude of event; Na8906; Natsushima; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; S2000; Sample ID; Sediment type; Shinkai2000_408-S1; Shinkai2000_408-S2; Shinkai2000_408-S3; Shinkai2000_408-S4; Shinkai2000_DV408; Size; Submersible Shinkai 2000; Substrate type; Uniform resource locator/link to image During Dive 408 of Shinkai 2000 on the flank of the Kaikata Seamount located on the volcanic front of the Izu-Ogasawara (Bonin) Arc, possibly recent hydrothermal manganese deposits were observed on sandy volcanic sediments at water depths of between 800 and 1200 m. The deposits cover almost the entire surface sediment across the manganese belt on the northwestern flank on the seamount on a scale of kilometers. The occurrence of the deposits, seafloor morphology and temperature of the sediments, together with previous shipboard results, lead to a possible model for the formation of the manganese deposits: A low-temperature hydrothermal solution ascends through fractures or faults in the volcanic substrate into permeable volcanic sands and precipitates manganate minerals which cement several centimeters of surface sand as hardpan. More intense and probably intermittent discharge of hydrothermal solution follows and forms many typical ridge-like vents and mounds on the seafloor. Subsequently, pure dense manganate layers developed beneath the semi-consolidated volcanic sandstone and act as a cap to the ascending fluids. The proposed mechanism may be the dominant type of low-temperature hydrothermal mineralization in submarine island-arc volcanoes and rifts. Similar hydrothermal manganese deopsits most probably occur in other active areas of the modern seafloors and in inactive island arcs. |
| title | Observation of manganese deposits on Kaikata Seamount, Izu-Ogasawara (Bonin) Arc by the Shikai 2000 submersible |
| topic | Date/Time of event; Deposit type; DEPTH, sediment/rock; Description; DV408/St_1; DV408/St_2; DV408/St_3; DV408/St_4; Elevation of event; Event label; Kaikata Seamount, Pacific Ocean; Latitude of event; Longitude of event; Na8906; Natsushima; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; S2000; Sample ID; Sediment type; Shinkai2000_408-S1; Shinkai2000_408-S2; Shinkai2000_408-S3; Shinkai2000_408-S4; Shinkai2000_DV408; Size; Submersible Shinkai 2000; Substrate type; Uniform resource locator/link to image |
| url | https://doi.org/10.1594/PANGAEA.880486 |