Gold Mineralization at the Forecast Hydrothermal Field in Southern Mariana Trough

DC Field Value Language
dc.contributor.author 최선기 -
dc.contributor.author 박상준 -
dc.contributor.author 박정우 -
dc.contributor.author 최상훈 -
dc.contributor.author 김종욱 -
dc.date.accessioned 2020-07-15T07:32:02Z -
dc.date.available 2020-07-15T07:32:02Z -
dc.date.created 2020-02-11 -
dc.date.issued 2019-08-22 -
dc.identifier.uri https://sciwatch.kiost.ac.kr/handle/2020.kiost/22422 -
dc.description.abstract Gold-rich (up to 72.6 ppm) massive sulfide and hydrothermally altered host rock were collected by remotely operated vehicle, HAEMIRE, from the Forecast hydrothermal field in Southern Mariana Trough. Gold-rich massive sulfide is featured by Zn-rich (up to 51.1 wt.%) ore, mainly composed of sphalerite, pyrite, chalcopyrite and galena with tennantite and electrum as minor minerals. The altered host rock can be subdivided into sulfide-rich part and altered silicate part. The sulfide-rich part is mainly composed of sphalerite and pyrite with minor chalcopyrite while XRD examination shows that montmorillonite ± anorthite are predominant in the altered silicate part. The FeS contents in sphalerite represent a decreasing trend as mineralization advanced (6.5 -
dc.description.uri 1 -
dc.language English -
dc.publisher Geochemical Society -
dc.relation.isPartOf Goldschmidt 2019 -
dc.title Gold Mineralization at the Forecast Hydrothermal Field in Southern Mariana Trough -
dc.type Conference -
dc.citation.conferencePlace US -
dc.citation.endPage 1 -
dc.citation.startPage 1 -
dc.citation.title Goldschmidt 2019 -
dc.contributor.alternativeName 최선기 -
dc.contributor.alternativeName 박상준 -
dc.contributor.alternativeName 김종욱 -
dc.identifier.bibliographicCitation Goldschmidt 2019, pp.1 -
dc.description.journalClass 1 -
Appears in Collections:
Marine Resources & Environment Research Division > Ocean Georesources Research Department > 2. Conference Papers
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