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,Marine Chemistry,1999.
[2]
刘长华,殷学博,关于现代浅海型海底热液活动的研究进展,地球科学进展,2006(9).
[3]
Letouzey J,Kimura M,Okinawa Trough genesis:structure and evolution of a back arc basin developed in a continent,Marine and Petroleum Geology,1985.
[4]
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,Proc Geol Soc China,1989(2).
[5]
Chen C H,Lee T,Shieh Y N,Magmatism at the onset of back-arc basin spreading in the Okinawa Trough,Journal of Volcanology and Geothermal Research,1995.
[6]
Chen Y G,Wu W S,Chen C H,A date for volcanic eruption inferred from a siltstone xenolith,Quaternary Science Reviews,2001.
[7]
郭富雯,龟山岛海底热液活动初步调查,中国台北:台湾中山大学,2001.
[8]
Von Damm K L,Edmond J M,Grant B,Chemistry of submarine hydrothermal solutions at 21°N,East Pacific Rise,Geochimica et Cosmochimica Acta,1985.
[9]
Bischoff J L,Dickson F W,Seawater-basalt interaction at 200℃ and 500 bars:Implications for origin of seawater heavy-metal deposits and regulation of seawater chemistry,Earth and Planetary Science Letters,1975.
[10]
Von Damm K L,Edmond J M,Measures C I,Chemistry of submarine hydrothermal solutions at Guaymas Basin,Gulf of California,Geochimica et Cosmochimica Acta,1985.
[11]
Von Damm K L,Seafloor hydrothermal activity:Black smoker chemistry and chimneys,Annual Review of Earth and Planetary Sciences,1990.
[12]
Sedwick P,Stuben D,Chemistry of shallow submarine warm springs in an arc-volcanic setting:Vulcano Island,Aeolian Archipelago,Italy,Marine Chemistry,1996.
[13]
McCarthy K T,Pichler T,Price R E,Geochemistry of Champagne Hot Springs shallow hydrothermal vent field and associated sediments,Dominica,Lesser Antilles,Chemical Geology,2005.
[14]
Prol-Ledesma R M,Canet C,Melgarejo J C,Cinnabar deposition in submarine coastal hydrothermal vents,Pacific margin of central Mexico,Economic Geology,2002(6).
[15]
Vidal V M V,Vidal F V,Isaacs J D,Coastal submarine hydrothermal activity off northern Baja California,Journal of Geophysical Research,1978(B4).
[16]
Valsami-Jones E,Baltatzis E,Bailey E H,The geochemistry of fluids from an active shallow submarine hydrothermal system:Milos island,Hellenic Volcanic Arc,Journal of Volcanology and Geothermal Research,2005.
[17]
Prol-Ledesma R M,Canet C,Torres-Vera M A,Vent fluid chemistry in Bah1′a Concepcio′n coastal submarine hydrothermal system,Baja California Sur,Mexico,Journal of Volcanology and Geothermal Research,2004.
[18]
Shanks III W C,Seyfried Jr W E,Stable isotope studies of vent fluids and chimney minerals,southern Juan de Fuca Ridge,sodium metasomatism and seawater sulfate reduction,Journal of Geophysical Research,1987.
[19]
郑永飞,陈江峰,稳定同位素地球化学,北京:科学出版社,2000.
[20]
IAEA GNIP Maps and Animations,International Atomic Energy Agency,Vienna 2008
[21]
Chen C T,Zeng Z G,Kuo F W,Tide-influenced acidic hydrothermal system offshore NE Taiwan,Chemical Geology,2005.
[22]
Chen C H,Shieh Y N,Lee T,Nd-Sr-O isotopic evidence for source contamination and unusual mantle component under Luzon Arc,Geochimica et Cosmochimica Acta,1990.
