叶凯，徐平. 山东荣城大疃榴辉岩成因岩石学研究,岩石学报，1992，8(1): 27-39
Ye, K. and Xu, P.Petrogenesis of eclogites and related rocks in Rongcheng County, Shandongprovince. Petrologia Sinica, 1992, 8(1): 27-39.
叶凯，从柏林. 荣城滕家集超高压变质钙硅酸盐岩的岩石学研究,科学通报，1995， 40：730－733。
Ye, K. and Cong, B.Petrology of ultrahigh-pressure metamorphic meta-calcsillicate rocks. ChineseScience Bulletin, 1995, 40: 730-733.
叶凯， 叶大年. 高铝榍石中P+Mg+F=Si+Al+HO特殊替代的高压效应,科学通报，1996，41(9):811-814。
Ye Kai and Ye Danian.Significance of phosphorous (P)- and magnesium (Mg)-bearing high-Al titanite inhigh-pressure marble from Yangguantun, Rongcheng County, Shandongprovince. Chinese Science Bulletin, 1996, 41(14): 1194-1197.
叶凯，平岛崇男等. 青岛仰口榴辉岩中粒间柯石英的发现及其意义,科学通报，1996，41(15):1407-1408。
Ye, K., et al. Significanceof the finding of interstitial coesite in eclogite at Yangkou, Qingdao,eastern China.Chinese Science Bulletin, 1996, 41(15): 1407-1408.
Ye Kai and Hirajima Takao.High-pressure marble at Yangguantun, Rongcheng County,Shandong Province, eastern China.Mineralogy and Petrology. 1996, 57: 151-165.
Ye Kai., Cong B and YeD.N. Ultrahigh-pressure P-bearing titanite from eclogite at Houshuichegou,Shandong Province, Eastern China. Scientia Geologica Sinic, 1997, 6(1): 7-18.
Ye, K., Cong, B.,Hirajima, T. and Banno, S. Tectonic implications of transitional eclogite fromHaiyangsuo, Rushan county, eastern Shandong Peninsula. ScientiaGeologica Sinica, 1998, 7(4): 493-500.
叶凯， 从柏林，平岛崇男，坂野升平.山东海阳所麻粒岩向过渡榴辉岩转化的变质动力学过程及其构造意义,岩石学报，1999，15(1): 21-36.
Ye, K., Cong, B.L.,Hirajima, T. and Banno, S. Transformation of granulite to transitional eclogitein metabasite from Haiyangsuo, eastern Shandong Peninsula.Petrologia Sinica, 1999, 15(1): 21-36.
Ye, K., Yao, Y., Katayama, I. And Maruyama, S. Largeareal extent of ultrahigh-pressure (UHP) metamorphism in the Sulu UHP terrane,eastern China:new implications from coesite and omphacite inclusions in zircon from graniticgneisses. Lithos, 2000，52: 157-164.
Ye, K., Cong, B. and Ye,D. N. The possible subduction of continental material to depths greater than 200 km. Nature, 2000, 407: 734-736.
叶凯. 大别山－苏鲁超高压变质带的矿物学和岩石学研究进展,矿物岩石地球化学通报，2001，20：141－147.
Ye, K., Liu, J.B., Cong,B. and Maruyama, S. Overpressures induced by coesite-quartz transition inzircon. American Mineralogist, 2001, 86: 1151-1155.
Liu, J.B., Ye, K.,Maruyama, S., Cong, B.L. and Fan, H.R. Mineral inclusions in zircon fromgenisses in the ultrahigh-pressure zone of the Dabie Mountains, China. Journalof Geology, 2001, 109: 523-535.
Ye, K., Liu, J.B., Cong,B.L., Ye, D., Xu, P., Omori, S. and Maruyama, S. Ultrahigh-Pressure (UHP)Low-Al Titanites from carbonate-bearing rocks in Dabieshan-Sulu UHP terrane,Eastern China. Am. Mineral., 2002, 87: 875-881.
Liu J.B and Ye K. Transformation of garnet epidote amphiboliteto eclogite, western Dabie Mountains, China. J.metamorphic Geol., 2004, 22, 383–394.
Chen, Y., Ye, K., Liu,J.B. & Sun, M. Multistage metamorphism of the Huangtuling granulite,Northern Dabie Orogen, eastern China:implications for the tectonometamorphic evolution of subducted lowercontinental crust. J. metamorphic Geol., 2006, 24, 633–654.
Chen, Y., Ye, K., Liu,J.B., Sun, M. 2008. Quantitative P–T–X constraints on orthopyroxene-bearing high-pressuregranulites in felsic–metapelitic rocks:evidence from the Huangtuling granulite, Dabieshan Orogen. J. metamorphicGeol., doi:10.1111/j.1525-1314. 2008. 00780. x
续海金，叶凯，马昌前. 北大别早白垩纪花岗岩类的和锆石'同位素及其构造意义. 岩石学报.2008, 0087-03.
宋衍茹，叶凯，续海金. 洋壳俯冲过程中的地幔楔上升对流：来自芝麻坊石榴子石二辉橄榄岩早期变质的证据. 岩石学报. 2009, 025-01: 147-158.
Ye, K., Song, Y.R., Chen,Y., Xu, H.J., Liu, J.B., Sun, M. 2009. Multistage metamorphism of orogenicgarnet–lherzolite from Zhimafang, Sulu UHP terrane, E. China: Implications for mantle wedge convection duringprogressive oceanic and continental subduction.Lithos, 109 (2009) 155–175.
Guo, S., Ye, K., Chen, Y.,Liu, J.B. 2009. A NORMALIZATION SOLUTION TO MASS TRANSFER ILLUSTRATION OFMULTIPLE PROGRESSIVELY ALTERED SAMPLES USING THE ISOCON DIAGRAM. EconomicGeology, v. 104, pp. 881–886.
