BIBLIOS

Tipo
Artigos em Revista

Tipo de Documento
Artigo Completo

Título
Serpentinization and its implications for ultramafic-hosted sulfide mineralization: A case study at the Tianzuo hydrothermal field, 63.5°E, Southwest Indian Ridge

Participantes na publicação
Teng Ding (Author)
Ágata Alveirinho Dias (Author)
Instituto Dom Luiz (IDL), Faculdade de Ciências, Universidade de Lisboa, Campo Grande, 1749–016, Lisboa, Portugal
Dep. Geologia
IDL
Jia Wang (Author)
Tingting Tan (Author)
Jin Liang (Author)
Bin Wu (Author)
Chunhui Tao (Author)

Resumo
Reaction of ultramafic rocks with seawater and subsequent serpentinization has been considered one of the most important factors controlling the formation of ultramafic-hosted seafloor massive sulfide (UM-SMS) deposits. However, the mineralization processes responsible for these deposits remain poorly understood, in particular because they are less abundant as compared with their basaltic counterparts. In this work, serpentinites with different alteration grades collected at the Tianzuo hydrothermal field (THF), Southwest Indian Ridge, were studied. Mineralogical and chemical analyses were performed in the secondary opaque minerals resulting from serpentinization to understand the role of this process during the formation of UM-SMS deposits. Our results show that these opaque minerals mainly consist of magnetite, hematite, pentlandite, and minor pyrite, suggestive of high but varying oxygen and sulfur fugacities. The hematite is characterized by an enrichment in Mg, Si, Ni, and Co as compared with magnetite. Pentlandite associated with hematite has elevated and consistent Ni contents as compared with that associated with magnetite. These results indicate that breakdown and decomposition of primary silicate and sulfide minerals during serpentinization has controlled the sources of ore-forming materials. Concentrations of Te are variable and show a positive correlation with Ni in pentlandite associated with magnetite or hematite, suggesting that gabbroic intrusions provided additional material to the hydrothermal system. Oxidation and sulfidation conditions are ideal for the formation of trisulfur ion S3− in THF, which can significantly improve the capability of hydrothermal fluids for leaching ore-forming metals from the wall rocks, promoting the formation of THF. In addition of reduced systems, hydrothermal fluids with high oxygen and sulfur fugacities triggered by extensive seawater infiltration can most likely also develop in ultramafic-hosted systems. These results suggest that the areas with well-developed fractures are promising candidates for further exploration of UM-SMS deposits along mid-oceanic ridges.


Instituição
FACULDADE DE CIÊNCIAS DA UNIVERSIDADE DE LISBOA

Suporte
Marine Geology

Identificadores da Publicação
ISSN - 0025-3227

Editora
Elsevier BV



Identificadores do Documento
DOI - https://doi.org/10.1016/j.margeo.2022.106969
URL - http://dx.doi.org/10.1016/j.margeo.2022.106969

Identificadores de Qualidade
SCIMAGO Q1 (2023) - 0.956 - Geology
SCIMAGO Q1 (2023) - 0.956 - Oceanography
SCOPUS Q1 (2023) - 6.1 - Geology
SCOPUS Q1 (2023) - 6.1 - Oceanography

Keywords
Tianzuo hydrothermal fieldUltramafic rocksSulfide mineralizationOpaque mineralsOxidation and sulfidation SMS deposits hydrothermal systems MOR SWIR Ultramafic hydrothermal processes hydrothermal processes

Tags
seafloor hydrothermal processes MOR SWIR