Guo F, Nakamuru E, Fan W M, Kobayoshi K and Li C W. 2007. Generation of Palaeocene Adakitic Andesites by Magma Mixing, Yanji Area, NE China. Journal of Petrology, 48(4): 661-692.
[16]
Jaques A L and Green D H. 1983. Anhydrous melting of peridotite at 0-15 kb pressure and the genesis of tholeiitic basalts. Contributions to Mineralogy and Petrology, 73: 287?310.
[17]
Kieffer B, Arndt N, Lapierre H, Bastien F, Bosch D, Pecher A, Yirgu G, Ayalew D, Weis D, Jerram D A, Keller F and Meugniot C. 2004. Flood and shied basalts from Ethiopia: Magmas from the African Superswell. Journal of Petrology, 45(4): 793-834.
[18]
Kushiro I. 2001 Partial melting experiments on peridotite and origin of mid-ocean ridge basalt. Annual Review of Earth and Planetary Sciences, 29: 71?107.
[19]
Menzies M A, Rogers N, Tindle A and Hawkesworth C J. 1987. Metasomatic and enrichment processes in lithospheric peridotites, an effect of asthenosphere- lithosphere interaction // Menzies M A and Hawkes?worth C J. Mantle Metasomatism. Academic Press, London: 313? 361.
[20]
Sun S S and McDonough W F. 1989. Chemical and isotopic systematics of oceanic basalts: Implication for mantle composition and processes // Saunders A D and Norry M J. Magmatism in the Ocean Basins. Geological Society, London, Special Publication, 42: 313?345.
[21]
Takahashi E, Shimazaki T, Tsuzaki Y and Yoshida H. 1993. Melting study of a peridotite KLB-1 to 6.5 GPa, and the origin of basaltic magmas. Philosophical Transactions of the Royal Society of London, A342: 105?120.
[22]
Taylor S R and McLennan S M. 1985. The Continental Crust: Its Composition and Evolution. Oxford: Blackwell: 312.
[23]
Weaver B L. 1991. The origin of ocean island basalts end-member compositions: Trace element and isotopic constraints. Earth and Planetary Science Letters, 104: 381?397.
[24]
Yang S F, Li Z L, Chen H L, Santosh M, Dong C W and Yu X. 2007. Permian bimodal dyke of Tarim Basin, NW China: Geochemical characteristics and tectonic implications. Gondwana Research, 12(1-2): 113?120
[25]
Zhang C L and Zhou H B. 2013. Comparison between the Permian mafic dykes in Tarim and the western part of Central Asian Orogenic Belt (CAOB), NW China: Implications for two mantle domains of the Permian Tarim Large Igneous Province. Lithos, 174: 15?27.
[26]
Zhang C L, Lu S N, Yu H F and Ye H M. 2007. Tectonic Evolution of Western Kunlun Orogenic Belt in Northern Qinghai-Tibet Plateau: Evidence from Zircon SHRIMP and LA-ICP-MS U-Pb Geochronology. Science China (Series D), 50(6): 825?835.
Condie K C. 2003. Incompatible element ratios in oceanic basalts and komatiites: Tracking deep mantle sources and continental growth rates with time. Geochemistry Geophysics Geosystems, 4 (1): 1525?2027.
[33]
Condie K C. 2005. High field strength element ratios in Archean basalts: A window to evolving sources of mantle plumes? Lithos, 79: 491?504.
[34]
Dupuy C, Liotard J M and Distal J. 1992. Zr/Hf fractionation in intraplate basaltic rocks: Carbonate metasomatism in the mantle source. Geochimica et Cosmochimica Acta, 56: 2417?2423.
[35]
Foley S. 1992. Vein-plus-wall-rock melting mechanisms in the lithosphere and the origin potassic alkaline magmas. Lithos, 28: 435 ?453.
[36]
Workman R K, Hart S R, Jackson M, Regelous M, Farley K A, Blusztajn J, Kurz M and Staudigel H. 2004. Recycled metasomatized lithosphere as the origin of the enriched mantle II (EM2) end-member: Evidence from the Samoan volcanic chain. Geochemistry Geophysics Geosystems, 5, Q04008, doi: 10.1029/2003GC000623.