共发表论文200余篇,合作出版专著5部。代表性论文有:[1]Blattner P, Hu RZ, et al., Temperatures and isotopic evolution of silicic magmas, Taupo Volcanic Zone and Coromandel, New Zealand, N. Z. J. Geol. Geophys., 1996, 39: 353-362.[2]Hu RZ, Burnard PG, et al., Helium and argon isotope systematics in fluid inclusions of Machangqing copper deposit in west Yunnan province, China, Chemical Geology, 1998, 146: 55-63.[3]Burnard PG, Hu RZ, et al., Mantle, crustal and atomspheric noble gases in Ailaoshan gold deposits, Yunnan province, China, Geochim. Cosmochim. Acta, 1999, 63: 1595-1604.[4]Hu RZ, Su WC, et al., Geology and geochemistry of Carlin-type gold deposits in China, Mineralium [5]Bi XW, Cornell DH, Hu RZ, REE composition of primary and altered feldspar from the mineralized alteration zone of alkali-rich intrusive rocks, western Yunnan province, China, Ore Geology Reviews, 2002,19: 69-78.[6]Fang WX, Hu RZ, et al., Influence of black shales on soils and edible plants in the Ankang area, Shanxi Province, China, Environmental Geochemistry and Health, 2002, 24: 35-46.[7]Peng JT, Hu RZ, et al., Samarium-Neodymium isotope systematics of hydrothermal calcites from the Xikuangshan antimony deposit (Hunan, China): The potential of calcite as a geochronometer, Chemical Geology, 2003, 200 : 129-136.[8]Hu RZ, Burnard PG, et al., Helium and argon isotope geochemistry of alkaline intrusion-associated gold and copper deposits along the Red River-Jinshajiang fault belt, SW China, Chemical Geology, 2004, 203:305-317.[9]Lee XQ, Hu RZ, et al., Ontogenetic trace element distribution in brachiopod shells: an indicator of original seawater chemistry, Chemical Geology, 2004, 209: 49-65.[10]Bi XW, Hu RZ, et al., The alkaline porphyry associated Yao'an gold deposit, Yunnan, China: rare earth element and stable isotope evidence for magmatic-hydrothermal ore formation, Mineralium Deposita, 2004,39:21-30.[11]Jia DC, Hu RZ, et al., Collision belt between the Kyanka block and the North China block in Yanbian region, Northeast China, Journal of Asian Earth Sciences,2004, 23: 211-219.[12]Zhao JH, Hu RZ, et al., Geochemistry, petrogenesis, and tectonic significance of Mesozoic mafic dikes, Fujian province, Southeastern China, International Geology Review, 2004, 46:542-557.[13]Zhong H, Hu RZ, et al., Review of the Link between the Hongges Layered Intrusion and Emeishan Flood Basalts, Southwest China: Internationgal Geology Review, 2005, 47, 971-985.[14]Liu S, Zou HB, Hu RZ, et al., Mesozoic mafic dikes from the Shandong Peninsula, North China Craton: Petrogenesis and tectonic implications, Geochemical Journal, 2006, 40: 181-195.[15]Li ZL, Hu RZ, et al., Helium isotope geochemistry of ore-forming fluids from Furong tin orefield in Hunan Province, China, Resource Geology, 2006, 56: 9-15.[16]Xie GQ, Hu RZ, et al., K-Ar dating, geochemical, and Sr-Nd-Pb isotopic systematics of late Mesozoic mafic dikes, southern Jiangxi Province, Southeast China: Petrogenesis and tectonic implications, International Geology Review, 2006, 48: 1023-1051.[17]Peng JT, Zhou MF, Hu RZ, et al., Precise molybdenite Re-Os and mica Ar-Ar dating of the Mesozoic Yaogangxian tungsten deposit, central Nanling district, South China, Mineralium Deposita, 2006, 41: 661-669.[18]Zhao JH, Hu RZ, et al., Elemental and Sr-Nd-Pb isotopic geochemistry of Mesozoic mafic intrusions in southern Fujian province, SE China: implications for lithospheric mantle evolution, Geological Magazine, 2007, 144: 937-952.[19]Li ZL, Hu RZ, et al., He, Pb and S isotopic constraints on the relationship between the A-type Qitianling granite and the Furong tin deposit, Hunan Province, China, Lithos, 2007, 97: 161-173.[20]Qi HW, Hu RZ, et al., Concentration and distribution of trace elements in lignite from the Shengli Coalfield, Inner Mongolia, China: Implications on origin of the associated Wulantuga Germanium Deposit, International Journal of Caol Geology, 2007, 71: 129-152.[21]Qi HW, Hu RZ, et al., REE Geochemistry of the Cretaceous lignite from Wulantuga Germanium Deposit, Inner Mongolia, Northeastern China, International Journal of Caol Geology, 2007, 71: 329-344.[22]Tao Y, Li CS, Hu RZ, et al., Petrogenesis of the Pt-Pd mineralized Jinbaoshan ultramafic intrusion in the Permian Emeishan Large Igneous Province, SW China, Contributions to Mineralogy and Petrology, 2007, 153: 321-337.[23]Hu RZ, Bi XW, et al., Uranium metallogenesis in South China and its relationship to crustal extension during the Cretaceous to Tertiary, Economic Geology, 2008, 103:583-598.[24]Liu S, Hu RZ, et al., U-Pb zircon age, geochemical and Sr-Nd-Pb-Hf isotopic constraints on age and origin of alkaline intrusions and associated mafic dikes from Sulu orogenic belt, Eastern China, Lithos, 2008, 106: 365-379.[25]Hu XY, Bi XW, Hu RZ, et al., Experimental study on tin partition between granitic silicate melt and coexisting aqueous fluid, Geochemical Journal, 2008, 42: 141-150.[26]Liu S, Hu RZ, et al., Zircon U-Pb geochronology and major, trace elemental and Sr-Nd-Pb isotopic geochemistry of mafic dykes in western Shandong Province, east China: Constrains on their petrogenesis and geodynamic significance, Chemical Geology, 2008, 255: 329-345.[27]Liu S, Hu RZ, et al., K-Ar ages and geochemical plus Sr-Nd isotopic compositions of adakitic volcanic rocks, western Shandong Province, eastern China: Foundering of the lower continental crust, International Geology Review, 2008, 50: 763-779.[28]Liu S, Hu RZ, et al., Cenozoic high Sr/Y volcanic rocks in the Qiangtang terrane, northern Tibet: geochemical and isotopic evidence for the origin of delaminated lower continental melts, Geological Magazine, 2008, 145: 463-474.[29]Yuan SD, Peng JT, Hu RZ, et al., A precise U-Pb age on cassiterite from the Xianghualing tin-polymetallic deposit (Hunan, South China), Mineralium Deposita, 2008, 43: 375-382.[30]Hu RZ, Burnard PG, et al., Mantle-derived gaseous components in ore-forming fluids of the Xiangshan uranium deposit, Jiangxi province, China: Evidence from He, Ar and C isotopes, Chemical Geology, 2009, 266: 86-95.[31]Hu RZ, Qi HW, et al., Geological and geochemical constraints on the origin of the giant Lincang coal seam-hosted germanium deposit, Yunnan, SW China: A review, Ore Geology Reviews, 2009, doi:10.1016/j.oregeorev.2009.02.007.[32]Liu S, Hu RZ, et al., Zircon U-Pb age, geochemistry and Sr-Nd-Pb isotopic compositions of adakitic volcanic rocks from Jiaodong, Shandong Province, Eastern China: Constraints on petrogenesis and implications, Journal of Asian Earth Sciences, 2009, 35: 445-458.[33]Zhong H, Zhu WG, Hu RZ, et al., Zircon U-Pb age and Sr-Nd-Hf isotope geochemistry of the Panzhihua A-type syenitic intrusion in the Emeishan large igneous province, southwest China and implications for growth of juvenile crust, Lithos, 2009, 110: 109-128.[34]Cao JJ, Hu RZ, et al., TEM observation of geogas-carried particles from the Changkeng concealed gold deposit, Guangdong Province, South China, Journal of Geochemical Exploration, 2009, 101: 247-253.[35]Bi XW, Hu RZ, et al., Crystallisation conditions (T, P, fO(2)) from mineral chemistry of Cu- and Au-mineralised alkaline intrusions in the Red River-Jinshajiang alkaline igneous belt, western Yunnan Province, China, Mineralogy and Petrology, 2009, 96: 43-58.[36]Su WC, Hu RZ, et al., Calcite Sm-Nd isochron age of the Shuiyindong Carlin-type gold deposit, Guizhou, China, Chemical Geology, 2009, 258: 269-274.