[1] Hollister C D, Ewing J I, Shipboard Scientists. Site 105: lower continental rise hills [M]. Initial Report DSDP, 1972,11:219-312.
[2] Corliss J B, Dymond J, Gordon L I, et al. Exploration of submarine thermal springs on the Galapagos Rift [J]. Science, 1979, 203:1 073-1 083.
[3] Campbell A C, Palmer M R, Klinkhammer G P, et al. Chemistry of hot springs on the Mid-Atlantic Ridge [J]. Nature, 1988, 335:514-519.
[4] Von Damm K L, Edmond J M, Grant B, et al. Chemistry of submarine hydrothermal solutions at 21°N, East Pacific Rise [J]. Geochimica Cosmochimica Acta, 1985, 49:2 197-2 220.
[5] Bowers T S, Campbell A C, Measures C I, et al. Chemical controls on the composition of vent fluids at 13°11 N and 21°N, East Pacific Rise [J]. Journal of Geophysical Research, 1988, 93: 4 522-4 536.
[6] Gamo T, Chiba H, Yamanaka T, et al. Chemical characteristics of newly discovered black smoker fluids and associated hydrothermal plumes at the Rodriguez Triple Junction, Central Indian Ridge [J]. Earth and Planetary Science Letters, 2001, 193: 371-379.
[7] Fouquet Y, Von Stackelberg U, Charlou J L, et al. Hydrothermal activity in the Lau Back-arc Basin-sulfides and water chemistry [J]. Geology, 1991, 19: 303-306.
[8] Grimaud D, Ishibashi J, Lagabrielle Y, et al. Chemistry of hydrothermal fluids from the 17°S active site on the North Fiji Basin Ridge (SW Pacific) [J]. Chemical Geology, 1991, 93: 209-218.
[9] McMurtry G M, Sedwick P N, Fryer P, et al. Unusual geochemistry of hydrothermal vents on submarine arc volcanoes-Kasuga Seamounts, Northern Mariana Arc [J]. Earth Planet Science Letters, 1993, 114: 517-528.
[10] Von Damm K L, Edmond J M, Measures C I, et al. Chemistry of submarine hydrothermal solutions at Guaymas Basin, Gulf of California [J]. Geochimica Cosmochimica Acta, 1985, 49:2 221-2 237.
[11] Pichler T, Veizer J, Hall E M G. The chemical composition of shallow-water hydrothermal fluids in Tutum Bay, Ambitle Island, Papua New Guinea and their effect on ambient seawater[J]. Marine Chemistry, 1999, 64: 229-252.
[12] Valsami-Jones E, Baltatzis E, Bailey E H. The geochemistry of fluids from an active shallow submarine hydrothermal system: Milos island, Hellenic Volcanic Arc [J]. Journal of Volcanology and Geothermal Research, 2005, 148: 130-151.
[13] Tarasov V G, Gebruk A V, Mironov A N, et al. Deep-sea and shallow-water hydrothermal vent communities: Two different phenomena? [J].Chemical Geology, 2005, 224: 5-39.
[14] Luan Xiwu. Distribution and tectonic environments of the hydrothermal fields [J]. Advances in Earth Science, 2004,19(6): 931-938.[栾锡武.现代海底热液活动区的分布与构造环境分析[J].地球科学进展,2004,19(6):931-938.]
[15] Von Damm K L. Seafloor hydrothermal activity: Black smoker chemistry and chimneys [J]. Annual Review Earth Planet Science,1990,18:173-204.
[16] McCarthy K T, Pichler T, Price R E. Geochemistry of Champagne Hot Springs shallow hydrothermal vent field and associated sediments, Dominica, Lesser Antilles[J]. Chemical Geology, 2005, 224:55-68.
[17] Sedwick P, Stuben D. Chemistry of shallow submarine warm springs in an arc-volcanic setting: Vulcano Island, Aeolian Archipelago, Italy [J]. Marine Chemistry, 1996, 53: 147-161.
[18] Pichler T. Stable and radiogenic isotopes as tracers for the origin, mixing and subsurface history of fluids in shallow-water hydrothermal systems [J]. Journal of Volcanology and Geothermal Research, 2005, 139(3/4):211-226.
[19] Bischoff J L, Seyfried W E. Hydrothermal chemistry of seawater from 25℃to 350℃ [J]. America Journal of Science, 1978, 278: 838-860.
[20] Zierenberg R A, Shanks W C, Bischoff J L. Massive sulfide deposits at 21°N, East Pacific Rise: Chemical composition, stable isotopes, and phase equilibria [J]. Geological Society of America Bulletin, 1984, 95: 922-929.
[21] Edmond J M, Jacobs S S, Gordon A L, et al. Water column anomalies in dissolved silica over opaline pelagic sediments and the origin of the deep silica maximum [J]. Journal of Geophysical Research-Oceans and Atmospheres, 1979, 84:7 809-7 826.
[22] Giggenbach W F. Isotopic shifts in waters from geothermal and volcanic systems along convergent plate boundaries and their origin[J]. Earth and Planetary Science Letters, 1992, 113: 495-510.
[23] Hedenquist J W. The thermal and geochemical structure of the Broadlands Ohaaki geothermal system, New Zealand [J]. Geothermics, 1990, 19: 151-185.
[24] Von Damm K L, Buttermore L G, Oosting S E, et al. Direct observation of the evolution of a seafloor "black smoker"from vapor to brine [J]. Earth and Planetary Science Letters, 1997, 149: 101-111.
[25] Prol-Ledesma R M. Similarities in the chemistry of shallow submarine hydrothermal vents [J]. Geothermics, 2003, 32: 639-644.
[26] Nahm G Y. Geology and groundwater resources of volcanic island, Cheju-do [J]. Geology and Ground-Water Resources, 1966, 3: 109-133.
[27] Brown L K. Gas Geochemistry of the Volcanic Hydrothermal Systems of Dominica and St. Lucia, Lesser Antilles: Implications for Volcanic Monitoring [M]. University of New Mexico, 2002.
[28] Chen C T, Zeng Z G, Kuo F W, et al. Tide-influenced acidic hydrothermal system offshore NE Taiwan [J]. Chemical Geology, 2005, 224: 69-81.
[29] Letouzey J, Kimura M. Okinawa Trough genesis: Structure and evolution of a back arc basin developed in a continent [J]. Marine Petrol Geology, 1985, 2: 111-130.
[30] Yeh Y H, Lin C H, Roecker S W. A study of upper crustal structures beneath northeastern Taiwan: Possible evidence of the western extension of Okinawa trough [J]. Proceedings of Geological Society China, 1989, 2: 139-156.
[31] Baubron J C, Allard P, Toutain J P. Diffuse volcanic emissions of carbon dioxide from Vulcano Island, Italy [J]. Nature, 1990, 344: 51-53.
[32] Rona P A. Hydrothermal mineralization at seafloor spreading centers [J]. Earth-Science Reviews, 1984, 20: 1-104.
[33] Alt J C. Hydrothermal oxide and nontronite deposits on seamounts in the Eastern Pacific [J]. Marine Geology, 1988, 81: 227-239.
[34] Hannington M, Herzig P, Stoffers P, et al. First observations of high-temperature submarine hydrothermal vents and massive anhydrite deposits off the north coast of Iceland [J]. Marine Geology, 2001, 177: 199-220.
[35] Pichler T, Veizer J. The precipitation of aragonite from shallow-water hydrothermal fluids in a coral reef, Tutum Bay, Ambitle Island, Papua New Guinea [J]. Chemical Geology, 2004,207:31-45.
[36] Pichler T, Veizer J. Precipitation of Fe(III) oxyhydroxide deposits from shallow-water hydrothermal fluids in Tutum Bay, Ambitle Island, Papua New Guinea [J]. Chemical Geology,1999, 162:15-31.
[37] Pichler T, Veizer J, Hall G E M. Natural input of arsenic into a coral-reef ecosystem by hydrothermal fluids and its removal by Fe(III) oxyhydroxides [J]. Environmental Science and Technology, 1999, 33 (9):1 373-1 378.
[38] Stuben D, Glasby G P. Geochemistry of shallow submarine hydrothermal fluids from Paleohori Bay, Milos, Aegean Sea [J]. Exploring Mining Geology, 1999, 8: 273-287.
[39] Johnson A, Cronan D S. Hydrothermal metalliferous sediments and waters off the Lesser Antilles [J]. Marine Georesources and Geotechnology, 2001, 19: 65-83.
[40] Millero F J, Sotolongo S, Izaguirre M. The oxidation kinetics of Fe(II) in seawater [J]. Geochimica Cosmochimica Acta, 1987, 51: 793-801.
[41] Chao T T, Theobald J P K. The significance of secondary iron and manganese oxides in geochemical exploration [J]. Economic Geology, 1976, 71: 1 560-1 569.
[42] Price R E, Pichler T. Distribution, speciation and bioavailability of arsenic in a shallow-water submarine hydrothermal system, Tutum Bay, Ambitle Island, PNG [J]. Chemical Geology, 2005, 224: 122-135.
[43] Pichler T, Dix G R. Hydrothermal venting within a coral reef ecosystem, Ambitle Island, Papua New Guinea [J]. Geology, 1996, 20 (5): 435-438.
[44] Pichler T, Giggenbach W F, McInnes B I A, et al. Fe-sulfide formation due to seawater gas sediment interaction in a shallow water hydrothermal system at Lihir Island, Papua New Guinea [J]. Economic Geology, 1999, 94: 281-288.
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