Formation of black and white smokers in the North Fiji Basin: Sulfur and lead isotope constraints

Title
Formation of black and white smokers in the North Fiji Basin: Sulfur and lead isotope constraints
Author(s)
김종욱; 이인성; 이경용; 유찬민; 고영탁
KIOST Author(s)
Kim, Jonguk(김종욱)Yoo, Chan Min(유찬민)Ko, Youngtak(고영탁)
Publication Year
2004-12-15
Abstract
The hydrothermal chimneys were recovered from 16o50’S triple junction area in the North Fiji Basin. The chimney samples are divided into three groups according to their mineralogy and metal contents; 1) Black smoker, 2) White smoker, 3) Transitional type. Black smoker chimneys are mainly composed of chalcopyrite and pyrite, and are enriched in high temperature elements such as Cu, Co, Mo, and Se. White smoker chimneys consist of sphalerite and marcasite with trace of pyrite and chalcopyrite, and are enriched in low temperature elements (Zn, Cd, Pb, As, and Ga). Transitional chimneys show intermediate characteristics in mineralogy and composition between black and white smokers. Basaltic rocks sampled from the triple junction show wide variation in geochemistry. Trace elements composition of basaltic rocks indicates that the magma genesis in the triple junction area was affected by mixing between N-MORB and E-MORB sources. The sulfur and lead isotope compositions of hydrothermal chimneys show distinct differences between the black and white smokers. Black smokers are depleted in 34S (δ34S = +0.4 to +4.8) and are low in lead isotope composition (206Pb/204Pb = 18.082 to 18.132; 207Pb/204Pb = 15.440 to 15.481; 208Pb/204Pb = 37.764 to 37.916) compared to white smoker and transitional chimneys (δ34S = +2.4 to +5.6; 206Pb/204Pb = 18.122 to 18.193; 207Pb/204Pb = 15.475 to 15.554; 208Pb/204Pb = 37.882 to 38.150). The heavier sulfur isotopic fractionation in white smoker can be explained by boiling of hydrothermal fluids and mixing with ambient seawater. The lead isotope compositions of the hydrothermal chimneys indicate that the metal in black and white smokers come from hydrothermal reaction with N-MORB and E-MORB, respectively. Regarding both black and white smoker are located in the same site, the condition of phase separation of hydrothermal fluid that formed white smokers might result from P-T condition of high temperature reaction zone below the hydrothermal venting
URI
https://sciwatch.kiost.ac.kr/handle/2020.kiost/31598
Bibliographic Citation
Eos. TRans. AGU / 2004 AGU Fall Meeting, 2004
Publisher
America Geophysical Union
Type
Conference
Language
English
Publisher
America Geophysical Union
Related Researcher
Research Interests

Ocean Geology,Mineral resources,해양지질,광물자원

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