Hou Z Q,Gao Y F,Qu X M,et al.Origin of adakitic intrusives generated during mid-Miocene east-west extension in southern Tibet[J].Earth Planet.Sci.Lett.,2004,220:139-155.
[7]
Hou Z Q,Ma H W,Zaw K,et al.The Himalayan Yulong porphyry copper belt:Product of large-scale strike-slip faulting in eastern Tibet[J].Economic Geology,2003,98:125-145.
[8]
Mo X X,Hou Z Q,Niu Y L,et al.Mande contributions to crustal thickening during continental collision:Evidence from Cenozoic igneous rocks in southern Tibet[J].Lithos,2007,96:225-242.
[9]
Liegeois J P.Preface:Some words on post-collisional magmatism[J].Lithos,1998,45:15-17.
[10]
Liegeois N P,Navez J,Hertogen J,et al.Contrasting origin of post-collisional high-K calc-alkaline and shoshonitic versus alkaline and peralkaline granitoids:The use of sliding normalization[J].Lithos,1998,45:1-28.
[11]
Harris N B W,Pearce J A,Tinde A G.Geochemical characteristics of collision zone magmatism[C]//Coward M P,Pies A C.Collision Tectonics.Ged.Soc.Specia Publication,1986,(19):67-81.
[12]
Bonin B,Azzouni-Sekkal A,Bussy F,et al.Alkali-calcic and alkaline post-orogenic (PO) granite magmatism:petrologic constraints and geodynamic settings[J].Lithos,1998,45:45-70.
[13]
Collins W J.Upper-and middle-crustal response to delamination:An example from the Lachlan fold belt,eastern Australia[J].Geology,1994,22:143-146.
[14]
Sylvester P J.Post-collisional alkaline granites[J].Journal of Geology,1989,97:261-280.
[15]
Sylvester P J.Post-collisional strongly peraluminous granites[J].Lithos,1998,45:29-44.
[16]
Solomovich L I.Postcollisional magmatism in the South Tien Shan Variscan Orogenic Belt,Kyrgyzstan:Evidence for high-temperature and high-pressure collision[J].Journal of Asian Earth Sciences,2007,30:142-153.
[17]
Wildner W,Lima E F,Nardi L V S,et al.Volcanic cycles and setting in the Neoproterozoic Ⅲ to Ordovician Camaqua Basin succession in southern Brazil:characteristics of post-collisional magmatism[J].Journal of Volcanology and Geothermal Research,2002,118:261-283.
Xiong X L,Adam T J,Green T H.Rutile stability and rutile/melt HFSE partitioning during partial melting of hydrous basalt:Implications for TTG genesis[J].Chemical Geology,2005,218:339-359.
[20]
张进江,丁林.青藏高原东西向伸展及其地质意义[J].地质科学,2003,38:179-189.
[21]
Xiao L,Clemens J D.Origin of potassic (C-type) adakite magmas:experimental and field constraints[J].Lithos,2007,95:399-414.
[22]
Whalen J B,Currie K L,Chappell B W.A-type granites:geochemical characteristics,discriminations and petrogenesis[J].Contributions to Mineralogy and Petrology,1987,95:407-419.
[23]
Eby G N.Chemical subdivision of the A-type granitoids:petrogenetic and tectonic implications[J].Geology,1992,20:641-644.
[24]
Wu F Y,Sun D Y,Li H M,et al.A-type granites in northeastern China:age and geochemical constraints on their petrogenesis[J].Chemical Geology,2002,187:143-173.
Tankut A,Wilson M,Yihunie T.Geochemistry and tectonic setting of Tertiary volcanism in the Guvem area,Anatolia,Turkey[J].Journal of Volcanology and Geothermal Research,1998,85:285-301.
[27]
Altunkaynak S,Genc S.Petrogenesis and time-progressive evolution of the Cenozoic continental volcanism in the Biga Peninsula,NW Anatolia (Turkey)[J].Lithos,2007(in press).
[28]
Varol E,Temel A,Gourgaud A,et al.Early Miocene adakite-like volcanism in the Balkuyumcu region,central Anatolia,Turkey:Petrology and geochemistry[J].Journal of Asian Earth Sciences,2007,30:613-628.
[29]
Aydogan M S,Ilbeyli N,Coban H,et al.Geochemical and isotopic(Nd,Sr) constraints on the petrogenesis of Baklan Granite in southem part of the Muratdag Region (Banaz,Usak),western Anatolia(Turkey)[J].Journal of Asian Earth Sciences,2007(in press).
[30]
Temel A,Gundogdu M N,Gourgaud A,et al.Ignimbrites of Cappadocia_Central Anatolia,Turkey:petrology and geochemistry[J].Journal of Volcanology and Geothermal Research,1998,85:447-471.
[31]
Kurkcuoglu B,Sen E,Aydar E,et al.Geochemical approach to magmatic evolution of Mt.Erciyes stratovolcano Central Anatolia,Turkey[J].Journal of Volcanology and Geothermal Research,1998,85:473-494.
[32]
Ozdemir Y,Karaoglu O,Tolluoglu A U,et al.Volcanostratigraphy and petrogenesis of the Nemrut stratovolcano (East Anatolian High Plateau):The most recent post-collisional volcanism in Turkey[J].Chemical Geology,2006,226:189-211.
[33]
Leite R.J,de Assis Janasi V,Creaser R A,et al.The late-to postorogenic transition in the Apia\' domain,SE Brazil:Constraints from the petrogenesis of the Neoproterozoic Agudos Grandes Granite Batholith[J].Journal of South American Earth Sciences,2007,23:213-235.
Zhu D C,Pan G T,Mo X X,et al.Petrogenesis of volcanic rocks in the Sangxiu Formation,central segment of Tethyan Himalaya:A probable example of plume-lithosphere interaction[J].Journal of Asian Earth Sciences,2007,29:320-335.
Rolland Y,Picard C,Pecher A,et al.The Cretaceous Ladakh arc of NW Himalaya:slab melting and melt-mantle interaction during fast northward drift of Indian Plate[J].Chemical Geology,2002,182:139-178.
Pearce J A,Harris B W,Tindle A G.Trace element discrimination diagrams for the tectonic interpretations of granitic rocks[J].J.Petrol.,1984,25:956-983.
[59]
de La Roche H,Leterrier J,Grandclaude P,et al.A classification of volcanic and plutonic rocks using R1-R2 diagram and major element analyses:Its relationships with current nomenclature[J].Chem.Geol.,1980,29:183-210.
[60]
Maniar P D,Piccoli P M.Tectonic discrimination of granitoids[J].Geol.Soc.Am.Bull.,1989,101:635-643.
[61]
Jiang Y H,Jiang S Y,Ling H F,et al.Low-degree melting of a metasomatized lithospheric mantle for the origin of Cenozoic Yulong monzogranite-porphyry,east Tibet:Geochemical and Sr-Nd-Pb-Hf isotopic constraints[J].Earth and Planetary Science Letters,2006,241:617-633.
[62]
Spurlin M S,Yin A,Horton B K,et al.Structural evolution of the Yushu-Nangqian region and its relationship to syncollisional igneous activity,east-central Tibet[J].GSA Bulletin,2005,117:1293-1317.
[63]
Williams H M,Turner S P,Pearce J A,et al.Nature of the source regions for post-collisional,potassic magmatism in southern and northern Tibet from geochemical variations and inverse trace element modelling[J].Journal of Petrology,2004,45:555-607.
Gao Y F,Hou Z Q,Kamber B S,et al.Adakite-like porphyries from the southern Tibetan continental collision zones:evidence for slab melt metasomatism ~].Contrib.Mineral.Petrol.,2007,153:105-120.
[67]
Guo Z F,Wilson M,Liu J Q.Post-collisional adakites in south Tibet:Products of partial melting of subduction-modified lower crust[J].Lithos,2007,96:205-224.
[68]
Qu X M,Hou Z Q,Li Y G.Melt components derived from a subducted slab in late orogenic ore-bearing porphyries in the Gangdese copper belt,southern Tibetan plateau[J].Lithos,2004,74:131-148.
[69]
Wang Q,McDermott F,Xu J F,et al.Cenozoic K-rich adakitic volcanic rocks in the Hohxil area,northern Tibet:Lowercrustal melting in an intracontinental setting[J].Geology,2005,33:465-468.
Visona D,Lombardo B.Two-mica and tourmaline leucogranites from the Everest-Makalu region (Nepal-Tibet):Himalayan leucogranite genesis by isobaric heating?[J].Lithos,2002,62:125-150.
Nelson K D.Are crustal thickness variations in old mountain belts like the Appalachians a consequence of lithospheric delamination?[J].Geology,1992,20:498-502.
Chung S L,Dunyi L,Ji J,et al.Adakites from continental collision zones:Melting of thickened lower crust beneath southern Tibet[J].Geology,2003,31:1021-1024.
[86]
Oyhantcabal P,Siegesmund S,Wemmer K,et al.Post-collisional transition from calc-alkaline to alkaline magmatism during transcurrent deformation in the southernmost Dom Feliciano Belt (Braziliano-Pan-African,Uruguay)[J].Lithos,2007(in press).
[87]
Turner S,Arnaud N,Liu J,et al.Post-collision,shoshonitic volcanism on the Tibetan plateau:implications for gonvective thinning of the lithosphere and the source of ocean island basalts[J],Journal of Petrology,1996,37:45-71.
