Mineralogy and geological significance of hydrothermal deposits from the Okinawa Trough

[1]  K. Nakashima,et al.  The Tiger Sulfide Chimney, Yonaguni Knoll IV Hydrothermal Field, Southern Okinawa Trough, Japan: The First Reported Occurrence of Pt–Cu–Fe‐Bearing Bismuthinite and Sn‐Bearing Chalcopyrite in an Active Seafloor Hydrothermal System , 2013 .

[2]  T. Oomori,et al.  Barite geochemistry from hydrothermal chimneys of the Okinawa Trough: insight into chimney formation and fluid/sediment interaction , 2011 .

[3]  Zhu Ji-hao Typomorphic Characteristics of Pyrite and Its Metallogenic Environment of Edmond Hydrothermal Field,Central Indian Ridge , 2011 .

[4]  Li Nai-sheng Mineralogy of Sulfides from Ultraslow Spreading Southwest Indian Ridge 49.6°E Hydrothermal Field and Its Metallogenic Significance , 2011 .

[5]  N. A. Semenov,et al.  Interaction in the MoSi2–W system at 1500 to 1800°C , 2009 .

[6]  W. Su,et al.  INVESTIGATION OF A NEW EXSOLVED CU-FE-S PHASE IN ABNORMAL SPHALERITE , 2009 .

[7]  U. Tsunogai,et al.  Diverse Range of Mineralization Induced by Phase Separation of Hydrothermal Fluid: Case Study of the Yonaguni Knoll IV Hydrothermal Field in the Okinawa Trough Back‐Arc Basin , 2008 .

[8]  Yun Liu,et al.  The crystal chemistry of Fe-bearing sphalerites: An infrared spectroscopic study , 2008 .

[9]  Cao Zhimin,et al.  Mineral Components, Texture, and Forming Conditions of Hydrothermal Chimney on the East Pacific Rise at 9°–10°N , 2007 .

[10]  Y. Fouquet,et al.  Mineralogy, geochemistry, and Nd isotope composition of the Rainbow hydrothermal field, Mid-Atlantic Ridge , 2006 .

[11]  H. Chiba,et al.  Tin-bearing chalcopyrite and platinum-bearing bismuthinite in the active Tiger chimney, Yonaguni Knoll IV seafloor hydrothermal system, South Okinawa Trough, Japan , 2005 .

[12]  Meng Xianwei,et al.  Rare earth element and strontium-neodymium isotope characteristics of hydrothermal chimney in Jade area in the Okinawa Trough , 2005 .

[13]  Qin Yunshan,et al.  Sulfur isotopic composition of seafloor hydrothermal sediment from the Jade hydrothermal field in the central Okinawa Trough and its geological significance , 2002 .

[14]  Hou Zengqian Rare Earth Element Geochemistry of Massive Sulphides from the Jade Hydrothermal Field in the Central Okinawa Trough , 2001 .

[15]  I. B. Butler,et al.  Framboidal pyrite formation via the oxidation of iron (II) monosulfide by hydrogen sulphide , 1999 .

[16]  M. Hannington,et al.  The internal structure of an active sea-floor massive sulphide deposit , 1995, Nature.

[17]  N. Cook,et al.  Sulphide mineralogy, metamorphism and deformation in the Matchless massive sulphide deposit, Namibia , 1994 .

[18]  P. Halbach,et al.  Geology and mineralogy of massive sulfide ores from the central Okinawa Trough, Japan , 1993 .

[19]  M. Kinoshita,et al.  Heat Flow Measurements in the Southern and Middle Okinawa Trough on R/V Sonne in 1988 , 1990 .

[20]  D. Janecky,et al.  Computational modeling of chemical and sulfur isotopic reaction processes in sea-floor hydrothermal systems; chimneys, massive sulfide, and subjacent alteration zones , 1988 .

[21]  U. Graham,et al.  Sulfide-sulfate chimneys on the East Pacific Rise, 11 degrees and 13 degrees N latitudes; Part I, Mineralogy and paragenesis , 1988 .

[22]  C. Lalou,et al.  Mineralogical zonation and radiochronological relations in a large sulfide chimney from the East Pacific Rise at 18 degrees 25'S , 1988 .

[23]  M. Hannington,et al.  Mineralogy and geochemistry of a hydrothermal silica-sulfide-sulfate spire in the caldera of Axial Seamount, Juan De Fuca Ridge , 1988 .

[24]  W. Shanks,et al.  Sulfur isotope study of chimney minerals and vent fluids from 21°N, East Pacific Rise: Hydrothermal sulfur sources and disequilibrium sulfate reduction , 1988 .

[25]  M. Yamano,et al.  Active hydrothermal mounds in the Okinawa Trough backarc basin, Japan , 1988 .

[26]  P. Bethke,et al.  Chalcopyrite disease in sphalerite : pathology and epidemiology , 1987 .

[27]  S. Scott Chemical behaviour of sphalerite and arsenopyrite in hydrothermal and metamorphic environments , 1983, Mineralogical Magazine.

[28]  R. Haymon Growth history of hydrothermal black smoker chimneys , 1983, Nature.

[29]  S. Sheppard,et al.  East Pacific Rise at latitude 21°N: isotopic composition and origin of the hydrothermal sulphur , 1981 .

[30]  G. Pantó,et al.  Electron-probe check of fe-distribution in sphalerite grains of the Nagybörzsöny hydrothermal ore deposits, Hungary , 1972 .

[31]  P. Ramdohr The ore minerals and their intergrowths , 1969 .