共 15 条
[1]
Themineralogy and the isotopic composition of sulfur inhydrothermal sulfide/sulfate deposits on the East Pa-cific Rise,21°N latitude. Styrt M M,Brackmann A J,Holland H D,et al. Earth and Planetary Science . 1981
[2]
Sulfur isotope study ofchimney minerals and vent fluids from 21°N,East Pa-cific Rise:Hydrothermal sulfur sources and disequi-librium sulfate reduction. Woodruff L G,Shanks W C. Journal of Geophysical Research . 1988
[3]
Origin of sulphur and geother-mometry of hydrothermal sulphides from the Galapa-gos Rift,86°W. Russell S,Max L C. Nature . 1982
[4]
Mineralogy and geo-chemistry of a hydrothermal silica-sulfide-sulfate spirein the caldera of Axial Seamount,Juan De Fuca Ridge. Hannington M D,Steven D S. The Canadian Mineralogist . 1988
[5]
Mineralogi-cal zonation and radiochronological relations in a largesulfide chimney from the East Pacific Rise at 18°25′S. Marchig V,Heinrich R,Claude L,et al. The Canadian Mineralogist . 1988
[6]
Growth history of hydrothermal blacksmoker chimneys. Rachel M H. Nature . 1983
[7]
Sulfideprecipitates at 21°N on the East Pacific Rise:226Ra,210Pb and210Po. Finkel R C,Macdougall J D,Chung Y C. Geophysical Research Letters . 1980
[8]
Hot spring deposits on theEast Pacific Rise at 21°N:preliminary description ofmineralogy and genesis. Rachel M H,Kastner M. Earth and Planetary Science . 1981
[9]
Evolution of an active sea-floormassive sulphide deposit. You C F,Bickle M J. Nature . 1998
[10]
Thecomposition of massive sulfide deposits from the sedi-ment-covered floor of Escanaba Trough,GordaRidge:implications for depositional processes. Randolph A K,Wayne C S,Wendy A B,et al. The Canadian Mineralogist . 1988