戴立群,戴立群.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. 戴立群,戴立群.Termination time of peak decratonization in North China: Geochemical evidence from mafic igneous rocks.LITHOS,2015,240327-336. 戴立群,戴立群.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. 戴立群,戴立群.The nature of orogenic lithospheric mantle: Geochemical constraints from postcollisional mafic-ultramafic rocks in the Dabie orogen.CHEMICAL GEOLOGY,2012,33499-121. 戴立群,戴立群.Geochemical insights into the role of metasomatic hornblendite in generating alkali basalts.GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS,2014,15(10):3762-3779. 戴立群,戴立群.Geochemical insights into the lithology of mantle sources for Cenozoic alkali basalts in West Qinling, China.LITHOS,2018,30286-98. 戴立群,戴立群.Recycling of Paleotethyan oceanic crust: Geochemical record from postcollisional mafic igneous rocks in the Tongbai-Hong'an orogens.GEOLOGICAL SOCIETY OF AMERICA BULLETIN,2016,129(1-2):179-192. 戴立群,戴立群.Geochemical Distinction between Carbonate and Silicate Metasomatism in Generating the Mantle Sources of Alkali Basalts.JOURNAL OF PETROLOGY,2017,58(5):863-884. 戴立群,戴立群.Postcollisional mafic igneous rocks record recycling of noble gases by deep subduction of the continental crust.LITHOS,2016,252135-144.