[1] Osborn E F. Role of oxygen pressure in the crystallization and differentiation of basaltic magmas[J]. American Journal of Science, 1959, 257: 609-647.[2] Bowen N L. The Evolution of the Igneous Rocks[M]. Princeton, New Jersey: Princeton University Press, 1928.
[3] Fenner C N. The crystallization of basalt[J]. American Journal of Science, 1929, 18: 223-253.
[4] Wiebe R A. Fractionation and liquid immiscibility in an anorthositic pluton of the Nain Complex, Labrador[J]. Journal of Ppetrology, 1979, 20: 239-269.[5] Ludden J N, Thompson G, Bryan W B, et al. The origin of lavas from the Ninetyeast Ridge, Eastern Indian Ocean: An evaluation of fractional crystallization models[J]. Journal of Geophysical Research, 1980, 85: 4 405-4 420.
[6] Fornari D J, Perfit M R, Malahoff A, et al. Geochemical studies of abyssal lavas recovered by DSRV Alvin from the Eastern Galapagos Rift, Inca Transform and Ecuador Rift. 1. Major element variations innatural glasses and spatial diatribution of lavas[J]. Journal of Geophysical Research, 1983, 88:10 519-10 529.
[7] Sinton J M, Wilson D S, Christie D M, et al. Petrologic consequences of rift propagation on oceanic spreading ridge[J]. Earth and Planetary Science Letters, 1983, 62: 193-207.
[8] Le Roex A P, Dick H J B. Petrography and geochemistry of basaltic rocks from the Conrad fracture zone on the America-Antarctica Ridge[J]. Earth and Planetary Science Letters, 1981, 54: 117-138.
[9] Le Roex A P, Dick H J B, Reid A M, et al. Ferrobasalts from the Spiess Ridge segment of the Southwest Indian Ridge[J]. Earth and Planetary Science Letters, 1982, 60:437-451.
[10] Brooks C K, Nielsen T F D. The East Greenland continental margin: A transition between oceanic and continental magmatism[J]. Geological Society of London Journal, 1982, 139: 265-275.[11] Bloomer S H, Natland J H, Fisher R L. Mineral relationships in gabbroic rocks from fracture zone of Indian Ocean ridges: Evidence for extensive fractionation, parental diversity and boundary layer recrystallization[A]. In: Saunders D D, Norry M T, eds. Magmatism in the Ocean Basins[C].Geological Society of London Special Publication, 1989, 42:107-124.
[12] Chalokwu C I, Ariskin A A, Koptev-Dvornikov E V. Magma dynamics at the base of an evolving mafic magma chamber: Incompatible element evidence from the Partridge River intrusion, Duluth Complex, Minnesota, USA[J]. Geochimica et Cosmochimica Acta, 1996, 60(24): 4 997-5 011.
[13] Lachize M, Lorand J P, Juteau T. Calc-alkaline differentiation trend in the plutonic sequence of the Wadi Haymiliyah section, Haylayn massif, Semail ophiolite, Oman[J]. Lithos, 1996, 38: 207-232.
[14] Brooks C K, Larsen L M, Nielsen T F D. Importance if iron-rich tholeiitic magma at divergent plate margins: A reappraisal[J]. Geology, 1991, 19:269-272.
[15] Leybourne M L, Van Wagoner N A, Ayers L D. Chenmical stratigraphy and petrogenesis of the early Preoterozoic Amisk Lake volcanic sequence, Flin Flon-Snow Lake Greenstone Belt, Canada[J]. Journal of Petrology, 1997, 38:1 541-1 564.
[16] Leybourne M L, Wangoner N V, Ayres L. Partial melting of a refracory subducted slab in a paleoproterozoic island arc: Implications for global chemical cycles[J]. Geology, 1999, 27(8):731-734.[17] Liao Chaolin, Wang Yuejun, Peng Touping. ⁴⁰Ar/³⁹Ar geochronology of paleoproterozoic mafic dykes from Southern Taihang Mountains and its geological significance[J]. Geotectonic et Metallogenia, 2003, 27(4):354-361. [廖超林, 王岳军, 彭头平. 太行山南段早元古代基性岩脉的⁴⁰Ar/³⁹Ar年代学及其构造意义[J].大地构造与成矿学, 2003, 27(4): 354-361.]
[18] Wang Y J, Fan W M, Zhang Y H, et al. Geochemical, ⁴⁰Ar/³⁹Ar geochronological and Sr-Nd isotopic constraints on the origin of Paleoproterozoic mafic dikes from the southern Taihang mountains and implications for the ca. 1800 Ma event of the North China Craton[J]. Precambrian Research,2004, 135: 55-77.
[19] Hanski E J, Smolkin V F. Iron and LREE-enriched mantle source for early Proterozoic intraplate magmatism as emplified by the Pechenga ferropicrites, Kola Peninsula, Russia[J]. Lithos, 1995, 34:107-125.
[20] Stone W E, Crockett J H, Dickin A P, et al. Origin of Archean ferropicrites geochemical constraints from the Boston Creek flow, Abitibi greenstone belt, Ontario, Canada[J]. Chemical Geology, 1995, 121: 51-71.
[21] Stone W E, Jensen L S, Church W R. Petrography and geochemistry of an unusual Fe-rich basaltic komatiite from Boaton Township, northeastern Ontario, Canada[J]. Journal of Earth Science, 1987, 24: 2 537-2 550.
[22] Wooden J L, Czamanske G K, Fedorenko V A, et al. Isotopic and trace-element constraints on mantle and crustal contributions to Siberian continental flood basalts, Noril'sk area, Siberia[J]. Geochimica et Cosmochimica Acta, 1993, 57:3 677-3 704.
[23] Lightfoot P C, Naldrett A J, Gorbachev N S, et al. Geochemistry of Siberian trap of the Noril'sk area, USSR, with implications for the relative contributions of crust and mantle to flood basalt magmatism[J]. Contributions to Mineralogy and Petrology, 1990, 104:631-644.
[24] Storey M, Mahoney J J, Saunders A D. Cretaceous basalts and the transition between plume and continental lithosphere mantle sources[J]. Geophysical Monograph, 1997, 100: 95-122.
[25] Ewart A, Milner S C, Armstrong R A, et al. Etendeka volcanism of the Goboboseb Mountains and Messum Igneous Complex, Namibia. Part I: Geochemical evidence of early Cretaceous Tristan plume melts and the role of crustal contamination in the Paran -Etendeka CFB[J]. Journal of Petrology, 1998, 39:191-225.
[26] Gibson S A. Major element heterogeneity in Archean to Recent mantle plume starting-heads[J]. Earth and Planetary Science Letters, 2002, 195: 59-74.
[27] Gibson S A, Thompson R N, Dickin A P. Ferropicrites: geochemical evidence for Fe-rich streaks in upwelling mantle plumes[J]. Earth and Planetary Science Letters, 2000, 174:355-374.
[28] Xu Yigang, Mei Houjun, Xu Jifeng, et al. Orogin of two differentiation trends in the Emeishan flood basalts[J]. Chinese Science Bulletin, 2003, 48(4): 383-387. [徐义刚, 梅厚钧, 许继峰,等.峨眉山大火成岩省中两类岩浆分异趋势及其成因[J]. 科学通报, 2003,48(4): 383-387.]
[29] Zhu Bingquan, Chang Xiangyang, Hu Yaoguo, et al. Discovery of Yanhe copper deposit in the Yunnan-Guizhou border area and a new train of thought for copper prospecting in the l arger igneous province of Emeishan flood basalts[J]. Advances in Earth Science, 2002,17（6）:912-917. [朱炳泉, 常向阳, 胡耀国, 等. 滇—黔边境鲁甸沿河铜矿床的发现与峨眉山大火成岩省找矿新思路[J]. 地球科学进展, 2002, 17(6):912-917.] 
[30] Brooks C K, Nielsen T F D. Early stages in the differentiation of the Skaergaard magma as revealed by a closely related suite of dike rocks[J]. Lithos, 1978, 11: 1-14.
[31] Halls H C, Li J H, Davis D, et al. A precisely dating Proterozoic palaeomagnetic pole from the North China craton, and its relevance to palaeocontinental reconstruction[J]. Geophysical Journal of International, 2000, 143:185-203.
[32] Hou Guiting, Li Jianghai, Qian Xianglin. Geochemical characteristics and tectonic setting of Meosoproterozoic dyk swarms in northern Shanxi[J]. Acta Petrologica Sinica, 2001, 17(3): 352-357. [侯贵廷, 李江海, 钱祥麟. 晋北地区中元古代岩墙群的地球化学特征和大地构造背景[J]. 岩石学报, 2001, 17(3):352-357.] 
[33] Wang Y J, Fan W M, Zhang Y H, et al. Structural evolution and ⁴⁰Ar/³⁹Ar dating of the Zanhuang metamorphic domain in North China Craton: Constraints on Paleo-proterozoic tectonothermal overprinting[J]. Precambrian Research, 2003,122:159-182.
[34] McCulloch M T. The role of subducted slabs in an evolving earth[J]. Earth and Planetary Science Letters, 1993, 115: 89-100.
[35] Tatsumi Y, Kogiso T. Trace element transport during dehydration processes in the subducted oceanic crust: 2. Origin of chemical and physical characteristics in arc magmatism[J]. Earth and Planetary Science Letters, 1997, 148: 207-221.
[36] Yogodzinski G M, Kelemen P B. Slab melting in the Aleutians: Implcations of an ion probe study of clinopyroxene in primitive adakite and basalt[J]. Earth and Planetary Science Letters, 1998, 158: 53-65.
[37] Clague D A, Frey F A, Thompson G, et al. Minor and trace element geochemistry of volcanic rocks dredged from the Galapagos Spreading Center: Role of crystal fractionation and mantle heterogeneity[J]. Journal of Geophysical Research, 1981, 86: 9 469-9 482.
[38] Dickey J S, Frey F A, Hart S R, et al. Geochemistry and petrology of dredged basalts from the Bouvet triple junction, South Atlantic[J]. Geochimica et Cosmochimica Acta, 1977, 41: 1 105-1 118.
[39] Christie D M, Sinton J M. Evolution of abyssal lavas along propagating segments of the Galapagos Sppreading Center[J]. Earth and Planetary Science Letters, 1981, 56: 321-335.
[40] Kennedy G C. Equilibrium between volatiles and iron oxides in igneous rocks[J]. American Journal of Science, 1948, 246: 529-549.
[41] Osborn E F. Role of oxygen pressure in the crystallization and differentiation of basaltic magmas[J]. American Journal of Science, 1959, 257: 609-647.
[42] Christie D M, Carmichael I S E, Langmuir C H. Oxidation states of mid-ocean ridge basalt glasses[J]. Earth and Planetary Science Letters, 1986, 79:397-411.
[43] Bryndzia L T, Wood B J, Dick H J B. The oxidation state of the Earth's sub-oceanic mantle from oxygen thermobarometry of abyssal spinel peridotites[J]. Nature, 1989, 341: 526-527.
[44] Wood B J, Bryndzia C T, Johnson K E. Mantle oxidation state and its relation to tectonic environments and fluid speciation[J]. Science, 1990, 245: 337-345.
[45] Juster T C, Grove T L, Perfit M R. Experimental constraints on the generation of Fe-Ti basalts, andesites and rhyodacites at the Galapagos spreading center, 85°W and 95°W[J]. Journal of Geophysical Research, 1989, 94:9 251-9 274.
[46] Larsen L M, Watt W S, Watt M. Geology and petrology of the lower Tertiary plateau basalts of the Scoresby Sund region, East Greenland[J]. Grønlands Geologiske Undersøgelse Bulletin, 1989, 157: 164.
[47] Herzberg C, Zhang J Z. Melting experiments on anhydrous peridotite KLB-1: Compositions of magmas in the upper mantle and ttansition zone[J]. Journal of Geophysical Research, 1996, 101:8 271-8 295.
[48] Polat A, Kerrich R, Wyman D A. The late Archean Schreiber-Hemlo and White River-Dayohessarah greenstone belts, Superior Province: Collages of Oceanic plateaus, oceanic arcs and subduction-accretion complexes[J]. Tectonophysics, 1998, 294:295-326.
[49] Kerrich R, Polat A, Wyman D A, et al. Trace element systematics of Mg- to Fe-tholeiitic basalt suites of the Superior Province: Implications for Archean mantle reserviors and greenstone belt genesis[J]. Lithos,1999, 46:163-187.
[50] Campbell I H, Griffiths R W. The changing nature of mantle hot spots through time: Implications for the chemical evolution of the mantle[J]. Journal of Geology, 1992, 92:497-523.
[51] Cordery M J, Davies G F, Campbell L H. Genesis of flood basalts from eclogite-bearing mantle plumes[J]. Journal Geophysical Research, 1997, 102:20 179-20 197.
[52] Takahasi E, Nakajima K, Wright T L. Origin of the Columbia River basalts: Melting model of a heterogeneous plume head[J]. Earth and Planetary Science Letters, 1998, 162:63-80.
[53] Yaxley G M. Experimental study of the phase and melting relations of homogeneous basalt+peridotite mixtures and implications for the petrogenesis of flood basalts[J]. Contribution to Mineralogy and Petrology, 2000, 139: 326-338.
[54] Yasuda A, Fujii T, Kurita K. Melting phase relations of an anhydrous mid-ocean ridge basalt from 3 to 20 GPa: Implications fro the behavious of subducted oceanic crust in the mantle[J]. Journal of Geophysical Research, 1994, 99:9 401-9 414.
[55] Laflèche M R, Dupuy C, Bougault H. Geochemistry and petrogenesis of Archean mafic volcanic rocks of the southern Abitibi Belt, Qu bec[J]. Precambrian Research, 1992, 57:207-241.
[56] Phinney W C, Halls H C. Petrogenesis of the early Proterozoic Matachewan dyke swarm, Canada and implication for magma emplacement and subsequent deformation[J]. Canada Journal of Earth Science, 2001, 38:1 541-1 563.