中国科学技术大学 dailiqun--Home--Scientific Research

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[1]dailiqun,dailiqun.Source and magma mixing processes in continental subduction factory: Geochemical evidence from postcollisional mafic igneous rocks in the Dabie orogen.GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS,2015,16(3):659-680.
[2]dailiqun,dailiqun.Termination time of peak decratonization in North China: Geochemical evidence from mafic igneous rocks.LITHOS,2015,240327-336.
[3]dailiqun,dailiqun.Tectonic development from oceanic subduction to continental collision: Geochemical evidence from postcollisional mafic rocks in the Hong'an-Dabie orogens.GONDWANA RESEARCH,2015,27(3):1236-1254.
[4]dailiqun,dailiqun.The nature of orogenic lithospheric mantle: Geochemical constraints from postcollisional mafic-ultramafic rocks in the Dabie orogen.CHEMICAL GEOLOGY,2012,33499-121.
[5]dailiqun,dailiqun.Geochemical insights into the role of metasomatic hornblendite in generating alkali basalts.GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS,2014,15(10):3762-3779.

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