Duchesne J C.1999.Fe-Ti deposits in Rogaland anorthosites (South Norway):geochemical characteristics and problems of interpretation.Mineralium Deposita,34:181 ~ 198.
[8]
Gauert C D K.1998.The petrogenesrs of the Uitkomst Complex,Mpumalanga Province,South Africa.Ph.D.theses unpubl.,University of Pretoria,South Africa,1~315.
[9]
He B,Xu Y,Xiao L,Chung S,et al.2003.Sedimentary evidence for a rapid,kilometer-scale crustal doming prior to the eruption of the Emeishan flood basalts.Earth Planet.Scie.Lett.,213:391~405.
[10]
Kyser T K,Carmeron W E,Nisbet E G.1986.Boninite petrogenesis and alteration history; constraints from stable isotope compositions of boninites from Caoe Vogel,New Caledonia and Cyprus.Contri.Mineral.Petrol.,93:222~226.
[11]
Mattey D,Lowry D,Macpherson C.1994.Oxygen isotope composition of mantle periotite.Earth Planet.Sci.Lett.,128,231~241.
[12]
Neal C R,Mahoney J J,Chazey W J.2002.Mantle sources and the highly variable role of continental lithosphere in basalt petrogenesis of the Kerguelen Plateau and Broken Ridge LIP:results from ODP Leg 183.J.Petrol.,43:1177~1205.
[13]
Sharma M A,Basu R,Nesterenko G V.1992.Temporal Sr-,Nd-,and Pb-isotopic variations in the Siberian flood basalts:implications for the plume-source characteristics.Earth Planet.Sci.Lett.,113:365~381.
[14]
Song X Y,Zhou M F,Hou Z Q.et al.2001.Geochemical constrains on the mantle source of the Upper Permian Emeishan Continental Flood Basalts,Southwestern China.International Geology Review,43:213~225.
[15]
Zhang Z,Mao J,Wang F,et al.2005.Mantle Plume Activity and Melting conditions:Evidences from Olivines in Picritic Rocks from the Emeishan Large Igneous Province,Southwestern China.Episodes,28(3):171~176.
[16]
Zhou M F,Robinson P T,Lesher C M,et al.2005.Geochemistry,petrogenesis and metallogenesis of the Panzhihua gabbroic layered intrusion and associated Fe-Ti-V oxide deposits,Sichuan Province,SW China,J.Petrol.,46:2253~2280.
Bhat I,Zainuddin S M.1981.The Panjal Trap chemistry; witness to the birth of Tethys.Geol.Mag.,118:355~365.
[25]
Chung S L & Jahn B.1995.Plume-lithosphere interaction in generation of the Emeishan flood basalts at the Permian-Triassic boundary.Geology,23:889~893.
[26]
Chung S L,Jahn B M,Wu G et al.1998.The Emeishan flood basalt in SW China; a mantle plume initiation model and its connection with continental breakup and mass extinction at the PerianTriassic boundary.In:Flower M F J,Chung S L,Lo C H & Lee T Y.eds.Mantle Dynamics and Plate Interactions in East Asia.AGU Geodynamics Series,27:47 ~ 58.
[27]
Gam S B,Mostert A B.1982.The Geological setting of the platinoid and base metal sulfide mineralization in the Platreef of the Bushveld Complex in Drenthe,north of Potgietersrus.Econ.Geol.,77:1395~1404.
[28]
Grinenko L N.1985.Sources of sulfur of the nickeliferous and barren gabbro-dolerite intrusions of the northwest Siberian platform.Int.Geol.Rev.,27:695~708.
[29]
Harmon R S,Kempton P D,Stosch H G,et al.1987.18O/16O ratios in anhydrous spinel lherzolite xenoliths from the SdhavarynTsaram volcano,Mongolia.Earth Planet.Sci.Lett.,81:193~202.
[30]
Haughton D R,Roeder P L,Skinner B J 1974.Solubility of sulphur in mafic magmas.Econ.Geol.,69:451~467.
[31]
Kamo S L,Czamanske G K,Amelin Y,et al.2003.Rapid eruption of Siberian flood-volcanic rocks,coincident with the PermianTriassic boundary and mass extinction at 251 Ma.Earth Planet.Sci.Lett.,214:75~91.
[32]
Lightfoot P C,Hawkesworth C J,et al.1993.Remobilisation of the continental lithosphere by a mantle plume:major-,trace element and Sr-,Nd-,and Pb-isotope evidence from picritic and tholeiitic lavas of the Noril\'sk District,Siberian Trap,Russia.Contrib.Mineral.Petrol.,114:171~188.
[33]
Naldrett A J,Lightfoot P C,Fedorenko V A,et al.1992.Geology and geochemistry of intrusions and flood basalts of the Noril\'sk Region,USSR,with implications for origin of the Ni-Cu ores.Econ.Geol.,87:975~1004.
[34]
Saunders A D,England R W,Reichow M K,et al.2005.A mantle plume origin for the Siberian Traps:uplift and extension in the West Siberian Basin,Russia.Lithos,79:407 ~ 424.
[35]
Sharpe M R 1981.The chronology of magma influxes to the eastern compartment,Bushveld Complex,as exemplified by its marginal border groups.Journal of Geological Society London,81:373~378.
[36]
Sun S S,McDonough W F.1989.Chemical and isotopic systematics of oceanic basalts:implications for mantle composition and processes.In:Saunders A D & Norry M J,ed.Magrnatism in the Ocean Basins.Geological Society.London,Special Publication,42:313~345.
[37]
Von Scherbler W H T M,Cawthorn R G,Kenyon A K,et al.1995.Nickel-Cu sulphide mineralization In the Uitkomst Intrusion.In..Extended Abstracts of the Cetennial Geocongress (1995).Geological Society of South Africa,Johannesburg,South Africa,133~1 36.
[38]
Xu Y,He B,Chung S L,et al.2004.Geologic,geochemical,and geophysical consequences of plume involvement in the Emeishan flood-basalt province.Geology,32; 917~920.
[39]
Zhang Zhaochong and Wang Fusheng,2002.Geochemistry of the two types of basalts of the Emeishan Basaltic Province:evidences for mantle plume-lithosphere interaction.Acta Geologica Sinica,76(2):138~147.
[40]
Zhou M F,Malpas J,Song X Y.2002.A temporal link between the Emeishan large igneous province (SW China) and the endGuadalupian mass extinction.Earth Planet.Sci.Lett.,196:113~122.