[1] Bi Xianwu, Hu Ruizhong and He Mingyou，Age determination of Ailaoshan gold metallogenic belt by ESR method and its geological significance, Chinese Science Bulletin, 1996, 41(18): 1546-1549.
[2] Bi Xianwu and Hu Ruizhong，REE geochemistry of primitive ore fluids in Ailaoshan gold belt, southwest China，Chinese Journal of Geochemistry，1998, 17(1): 91-96.
[3] Bi Xianwu，Mantle–derived sulfur and its time constraints on gold mineralization of Ailaoshan gold belt, China, Chinese Science Bulletin, 1999, 44(supp): 242-244.
[4] Bi Xianwu, Hu Ruizhong, Ye Zaojun, and Shao Shuxun，Study on the relations between A-type granites and copper mineralization as exemplied by the Machangqing Cu deposit, Science in China (Series D), 2000, 43(1): 93-102.
[5] Bi Xianwu, Cornell D. H., and Hu Ruizhong, 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] Bi Xianwu, Hu Ruizhong, D. H. Cornell et al.,Trace element and isotope evidence for the evolution of ore-forming fluid of Yao’an gold deposit,Yunnan province, China, Mineralium Deposita, 2004, 39: 21-30
[7] Bi Xianwu, Hu Ruizhong, Mungall JE, Hanley JJ, Mineral chemistry studies on crystallization conditions (T, P, fO2) of Cu-Au mineralized alkaline intrusions in Ailaoshan-Jinshajiang alkaline intrusion blet, western Yunnan, China. Mineralogy and Petrology, 2009, 96: 43-58
[8] Hu Xiaoyan, Bi Xianwu, Hu Ruizhong, Shang Linbo, Fan Wenling, Experimental study on tin partition between granitic silicate melt and coexisting aqueous fluid, Geochemical Journal, 2008, 42(2):141-150.
[9] Hu Ruizhong, Bi Xianwu, He Mingyou, Liu Bingguang, Turner G., and Burnard P.G.，Mineralizer constraint on gold mineralization of Ailaoshan gold belt, Science in China (Series D), 1998, 41(supp): 74-82.
[10] Shang LB, Bi XW, Hu RZ, Fan WL，An experimental study on the solubility of copper bichloride in water vapor, Chinese Science Bulletin, 2007, 52 (3): 395-400.
[11] Hu Ruizhong, Bi Xianwu, and Zhou Meifu et al., 2006, Carbon isotopic geochemistry of uranium deposits in South China: constraints on the regional uranium mineralization, Economic Geology (in reviews)
[12] Hu Ruizhong, Burnard PG, Bi Xianwu, Zhou Meifu, Peng Jiantang, Su Wenchao, Wu Kaixing，Helium and argon isotope geochemistry of alkaline intrusion-associated gold and copper deposits along Red River – Jinshajiang fault belt, SW China, Chemical Geology, 2004, 203: 305-317.
[13] 毕献武、胡瑞忠、彭建堂、吴开兴、战新志，姚安和马厂箐富碱侵入岩体岩石地球化学特征，岩石学报，2005，21(1): 113-124.
[14] 李鸿莉、毕献武、涂光炽、胡瑞忠，芙蓉锡矿田骑田岭花岗岩黑云母矿物化学及其对锡成矿的指示意义，岩石学报，2007，23(10)：
[15] 毕献武、胡瑞忠、何明友，哀牢山金矿带ESR年龄及其地质意义，科学通报，1996, 41(14): 1301-1303.
[16] 毕献武、胡瑞忠，墨江金矿成矿流体的形成演化机制，地质论评，1997, 43(4): 381-387.
[17] 毕献武、胡瑞忠，哀牢山金矿带主要金矿床成矿流体特征，矿物学报，1997, 17(4): 435-441.
[18] 毕献武、胡瑞忠，哀牢山金矿带成矿流体稀土元素地球化学，地质论评，1998, 44(3): 264-269.
[19] 毕献武、胡瑞忠，大坪金矿成矿机理探讨，矿物学报，1999, 19 (1):28-33.
[20] 毕献武、胡瑞忠、叶造军、邵树勋，A型花岗岩类与铜成矿关系研究—以马厂箐铜矿为例，中国科学（D辑），1999, 29(6): 489-495.
[21] 毕献武、胡瑞忠、D. H. Cornell，蚀变流体的来源：矿化蚀变带中原生与次生长石的REE证据，科学通报，2000，45 (13): 1429-1432.
[22] 毕献武、胡瑞忠、黄铁矿微量元素地球化学特征及其对成矿流体性质的指示，矿物岩石地球化学通报，2004
[23] 毕献武、胡瑞忠、Hanley JJ、Mungall JE、彭建堂、吴开兴、李鸿莉，与铜、金矿化有关的富碱侵入岩矿物化学研究，矿物学报，2006，26(4)：377-386.
[24] 毕献武等，骑田岭A型花岗岩流体包裹体地球化学特征——对芙蓉超大型锡矿成矿流体来源的指示，高校地质学报，2008.
[25] 李鸿莉、毕献武、涂光炽、胡瑞忠，岩背花岗岩体黑云母矿物化学研究及其对成岩成矿意义的指示，矿物岩石，2007，
[26] 胡瑞忠、毕献武、 Turner G.、Burnard P.G.，哀牢山金矿带金成矿流体He-Ar同位素地球化学，中国科学（D辑），1999，29(4):321-330.
