Becker H,Jochum K P,Carlson R W.2000.Trace element fractionation during dehydration of eclogites from high-pressure terranes and the implications for element fluxes in subduction zones.Chemical Geology,163:65~99.
[4]
Davies J H.1999.The role of hydraulic fractures and intermediate-depth earthquakes in generating subduction-zone magmatism.Nature,398:142~145.
[5]
Gao J,Klemd R.2001.Primary fluids entrapped at blueschist to eclogite transition:evidence from the Tianshan meta-subduction complex in northwestern China.Contributions to Mineralogy and Petrology,142:1~14.
[6]
Gao J,Klemd R.2003.Formation of HP-LT rocks and their tectonic implications in the western Tianshan Orogen,NW China:geochemical and age constraints.Lithos,66:1~22.
[7]
Hacker B R,Peacock S M,Abers G A,et al.2003.Subduction factory 2.Are intermediate-depth earthquakes in subducting slabs linked to metamorphic dehydration reactions? Journal of Geophysical Research,108(B1):2030~2046.
[8]
Hofmann A W.1988.Chemical differentiation of the earth:the relationship between mantle,continental crust and oceanic crust.Earth and Planetary Science Letters,90:297~314.
[9]
John T,Scherer E E,Haase K,et al.2004.Trace element fractionation during fluid-induced eclogitization in a subducting slab:trace element and Lu-Hf-Sm-Nd isotope systematics.Earth and Planetary Science Letters.227:441~456.
[10]
Manning C E.2004.The chemistry of subduction-zone fluids.Earth and Planetary Science Letters,223:1~16.
[11]
McCulloch M T,Gamble J A.1991.Geochemical and geodynamical constraints on subduction zone magmatism.Earth and Planetary Science Letters,102:358~374.
[12]
Rudnick R L,Barth M,Horn I,et al.2000.Rutile-bearing refractory eclogites:missing link between continents and depleted mantle.Science,287:278~281.
[13]
Rubatto D,Hermann J.2003.Zircon formation during fluid circulation in eclogites (Monviso,Western Alps):implications for Zr and Hf budget in subduction zones.Geochimica et Cosmochimica Acta,67(12):2173~2187.
[14]
Schmidt M W,Poli S.1998.Experimentally based water budgets for dehydrating slabs and consequences for arc magma generation.Earth and Planetary Science Letters,163:361~379.
[15]
Sun S-S,McDonough W F.1989.Chemical and isotopic systematics of oceanic basalts:implications for mantle composition and processes.In:Saunders A D,Dorry M J,eds.Magmatism in the Ocean Basins.London:Geological Society of London,42:313~345.
[16]
Tatsumi Y,Hamilton D L,Nesbitt R W.1986.Chemical characteristics of fluid phase released from a subducted lithosphere and origin of arc magmas:evidence from high-pressure experiments and natural rocks.Journal of Volcanology and Geothermal Research,29:293~309.
[17]
Tribuzio R,Messiga B,Vannucci R,et al.1996.Rare earth element redistribution during high-pressure low-temperature metamorphism in ophiolitic Fe-gabbros (Liguria,northwestern Italy):implications for light REE mobility in subduction zooes.Geology,24:711~714.
[18]
Volkova N I,Budanov V I.1999.Geochemical discrimination of metabasalt rocks of the Fan-Karategin transitional blueschist/greenschist belt,South Tianshan,Tajikistan:seamount volcanism and accretionary tectonics.Lithos,47:201~216.
[19]
Zack T,Rivers T,Foley S F.2001.Cs-Rb-Ba systematics in phengite and amphibole:an assessment of fluid mobility at 2.0 GPa in eclogites from Trescolmen,Central Alps.Contributions to Mineralogy and Petrology,140:651~669.
[20]
Zhang L,Ellis D J,Williams S,et al.2002b.Ultra-high pressure metamorphism in western Tianshan,China:Part II.Evidence from magnesite in eclogite.American Mineralogist,87:861~866.
Becker H,Jochum K P,Carlson R W.1999.Constraints from high-pressure veins in eclogites on the composition of hydrous fluids in subduction zones.Chemical Geology,160:291~308.
[24]
Boynton W V.1984.Geochemistry of the rare earth elements:meteorite studies.In:Henderson P,Ed.Rare Earth Element Geochemistry.New York:Elsevier,63~114.
[25]
Chan L H,Alt J C,Teagle D A H.2002.Lithium and lithium isotope profiles through the upper oceanic crust:a study of seawater-basalt exchange at ODP Sites 504B and 896A.Earth and Planetary Science Letters,201:187~201.
[26]
Gao J,He G,Li M,et al.1995.The mineralogy,petrology,metamorphic PTDt trajectory and exhumation mechanism of blueschists,south Tianshan,northwestern China.Tectonophysics,250:151~168.
[27]
Gao J,Klemd R,Zhang L,et al.1999.P-T path of high-pressure/low-temperaturerocks and tectonic implications in the western Tianshan Mountains,NW China.Journal of Metamorphic Geology,17:621~636.
[28]
Gao J,Xiao W,Li J,et al.2002.\'Central-Asia type\' Orogenesis and Metallogenesis in western China.IGCP-420 Workshop,August 5-14,Changchun,China,Abstracts and excursion guidebook,39.
[29]
Hofmann A W,Jochum K P,Seufert M,et al.1986.Nb and Pb in oceanic basalts:new constraints on mantle evolution.Earth and Planetary Science Letters,79:33~45.
[30]
Klemd R,Schroter F C,Will T M,et al.2002.P-T evolution of glaucophane-omphacite bearing HP-LT rocks in the western Tianshan Orogen,NW China:new evidence for \'Alpine-type\' tectonics.Journal of Metamorphic Geology,20:239~254.
[31]
Peacock S M.1993.The importance of blueschist → eclogite dehydration reactions in subducting oceanic crust.Geological Society of America Bulletin,105:684~694.
[32]
Stalder R,Foley S F,Brey G P,et al.1998.Mineral-aqueous fluid partitioning of trace elements at 900~1200°C and 3.0~5.7 GPa:new experimental data for garnet,clinopyroxene,and rutile,and implications for mantle metasomatism.Geochimica et Cosmochimica Acta,62(10):1781~1801.
[33]
Wei C J,Powell R,Zhang L F.2003.Eclogites from the south Tienshan,NW China:petrological characteristic and calculated mineral equilibria in the Na2O-CaO-FeO-MgO-Al2O3-SiO2-H2O system.Journal of Metamorphic Geology,21:163~179.
[34]
Zhang L,Ellis D J,Jiang W.2002a.Ultrahigh-pressure metamorphism in western Tianshan,China:Part I.Evidence from inclusions of coesite pseudomorphs in garnet and from quartz exsolution lamellae in omphacite in eclogites.American Mineralogist,87:853~860.