Metal-bearing molten sulfur collected from a submarine volcano: Implications for vapor transport of metals in seafloor hydrothermal systems SCIE SCOPUS

DC Field Value Language
dc.contributor.author Kim, Jonguk -
dc.contributor.author Lee, Kyeong-Yong -
dc.contributor.author Kim, Jung-Hoon -
dc.date.accessioned 2020-04-20T07:43:59Z -
dc.date.available 2020-04-20T07:43:59Z -
dc.date.created 2020-01-28 -
dc.date.issued 2011-04 -
dc.identifier.issn 0091-7613 -
dc.identifier.uri https://sciwatch.kiost.ac.kr/handle/2020.kiost/3877 -
dc.description.abstract Gray, metal-bearing molten sulfur was collected from the central volcanic cone of an active off-axis caldera (MTJ-1) in the northeastern Lau Basin, southwestern Pacific Ocean, during an expedition for hydrothermal vents undertaken by the Korea Deep Ocean Study (KODOS) program in 2006. The molten sulfur enveloped the frame and chain bag of the dredge at a depth of similar to 1700 m. Microscopically, the sulfur matrix contains numerous covellite (CuS) inclusions of various sizes and irregular shapes, indicating their formation via volcanic sublimation. The molten sulfur is enriched in elements commonly associated with magmatic input, including Cu, As, Au, Bi, Te, and Sb. The low sulfur isotope composition of the sulfur (delta S-34 = -7.5% to -8.2%) indicates an origin via the magmatic degassing of SO2 and disproportionation. The present results represent field-scale evidence for metal transport via sulfur-rich volcanic degassing in submarine massive sulfide deposits. The molten sulfur deposit plays an important role in enhancing the efficiency of the transfer of magmatic fluid to the hydrothermal system. -
dc.description.uri 1 -
dc.language English -
dc.publisher GEOLOGICAL SOC AMER, INC -
dc.subject HIGH-TEMPERATURE -
dc.subject WESTERN PACIFIC -
dc.subject GOLD DEPOSITS -
dc.subject CRATER LAKE -
dc.subject COPPER -
dc.subject FLUIDS -
dc.subject BASIN -
dc.subject ARC -
dc.title Metal-bearing molten sulfur collected from a submarine volcano: Implications for vapor transport of metals in seafloor hydrothermal systems -
dc.type Article -
dc.citation.endPage 354 -
dc.citation.startPage 351 -
dc.citation.title GEOLOGY -
dc.citation.volume 39 -
dc.citation.number 4 -
dc.identifier.bibliographicCitation GEOLOGY, v.39, no.4, pp.351 - 354 -
dc.identifier.doi 10.1130/G31665.1 -
dc.identifier.scopusid 2-s2.0-79954595982 -
dc.identifier.wosid 000288507300016 -
dc.type.docType Article -
dc.description.journalClass 1 -
dc.subject.keywordPlus HIGH-TEMPERATURE -
dc.subject.keywordPlus WESTERN PACIFIC -
dc.subject.keywordPlus GOLD DEPOSITS -
dc.subject.keywordPlus CRATER LAKE -
dc.subject.keywordPlus COPPER -
dc.subject.keywordPlus FLUIDS -
dc.subject.keywordPlus BASIN -
dc.subject.keywordPlus ARC -
dc.relation.journalWebOfScienceCategory Geology -
dc.description.journalRegisteredClass scie -
dc.description.journalRegisteredClass scopus -
dc.relation.journalResearchArea Geology -
Appears in Collections:
Marine Resources Research Division > Deep-sea Mineral Resources Research Center > 1. Journal Articles
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