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代表论著：
[1]LengCB,ZhangXC,HuangZL,HuangQY,WangSX,MaDY,ZhuZQ,LuoTY,LiC,LiWB,Geology,Re-Osages,sulfurandleadisotopesoftheDiyanqinamuporphyryModeposit,InnerMongolia,NEChina,EconomicGeology(inpress)
[2]LengCB,Huang,QY,ZhangXC,WangSX,Zhong,H,HuRZ,BiXW,ZhuJJ,WangXS.2014.PetrogenesisoftheLateTriassicvolcanicrocksinthesouthernYidunarc,SWChina:Constraintsfromthegeochronology,geochemistry,andSr-Nd-Pb-Hfisotopes.Lithos,90-191：363-382.
[3]LengCB,ZhangXC,ZhongH,HuRZ,ZhouWD,DuAD,QuWJ.2013.Re–OsmolybdeniteagesandzirconHfisotopesoftheGangjiangporphyryCu–ModepositintheTibetanOrogen.MineraliumDeposita,48:585-602,2013.
[4]LengCB,ZhangXC,HuRZ,WangSX,ZhongH,WangWQ,BiXW.2012.ZirconU-PbandmolybdeniteRe-OsGeochronologyandSr-Nd-Pb-HfisotopicconstraintsonthegenesisoftheXuejipingporphyrycopperdepositinZhongdian,NorthwestYunnan,China.JournalofAsianEarthSciencs,60:31-48,2012.
[5]WangSX,BiXW,LengCB,ZhongH,TangHF,ChenYW,YinGH,HuangDZ,ZhouMF.2014.GeochronologyandgeochemistryofLateCretaceousigneousintrusionsandMo–Cu–(W)mineralizationinthesouthernYidunArc,SWChina:Implicationsformetallogenesisandgeodynamicsetting,OreGeologyReviewers,61:73-95
[6]WangXS,HuRZ,BiXW,LengCB,PanLC,ZhuJJ,ChenYW,2014,PetrogenesisofLateCretaceousI-typegranitesinthesouthernYidunTerrane:NewconstraintsontheLateMesozoictectonicevolutionoftheeasternTibetanPlateau,Lithos,208–209:202–219.
[7]SunHR,HuangZL,LiWB,LengCB,MaDY,ZhangXC,2014,Chronology,geochemistryandSr–NdisotopestudiesofJurassicintrusionsintheDiyanqinamuporphyryMomine,centralInnerMongolia,China,JournalofAsianEarthSciences,88:85-97.
[8]ZhangY,TangHS,ChenYJ,LengCB,ZhaoCH,2014,Oregeology,fluidinclusionandisotopegeochemistryoftheXunyangHg–Sborefield,QinlingOrogen,CentralChina,GeologicalJournal,DOI:10.1002/gj.2560
[9]冷成彪,张兴春,秦朝建,王守旭,任涛,王外全.滇西北雪鸡坪斑岩铜矿流体包裹体初步研究.岩石学报,2008,09:2017-2028.
[10]冷成彪,张兴春,周维德.西藏尼木地区岗讲斑岩铜-钼矿床地质特征及锆石U-Pb年龄.地学前缘,2010,02:185-197.
[11]冷成彪,张兴春,王守旭,秦朝建,吴孔文,任涛.岩浆—热液体系成矿流体演化及其金属元素气相迁移研究进展.地质论评,2009,1:100-112.
[12]冷成彪,张兴春,王守旭,秦朝建,苟体忠,王外全.滇西北中甸松诺含矿斑岩的锆石SHRIMPU-Pb年龄及地质意义.大地构造与成矿学,2008,1:124-130.
[13]冷成彪,张兴春,王守旭,王外全,秦朝建,吴孔文,任涛.滇西北雪鸡坪斑岩铜矿S,Pb同位素组成及对成矿物质来源的示踪.矿物岩石,2008,4:80-88.
[14]冷成彪,张兴春,陈衍景,王守旭,苟体忠,陈伟.中国斑岩铜矿与埃达克(质)岩关系探讨.地学前缘,2007,05:199-210.
[15]冷成彪,张兴春,王守旭,秦朝建,苟体忠.云南中甸地区两个斑岩铜矿容矿斑岩的地球化学特征——以雪鸡坪和普朗斑岩铜矿床为例.矿物学报,2007,Z1:414-422.
[16]王守旭,张兴春,冷成彪,秦朝建,马德云,王外全.滇西北普朗斑岩铜矿锆石离子探针U-Pb年龄:成矿时限及地质意义.岩石学报,2008,10:2313-2321.
[17]王守旭,张兴春,冷成彪,秦朝建,王外全,赵茂春.中甸红山矽卡岩铜矿稳定同位素特征及其对成矿过程的指示.岩石学报,2008,03:480-488.
[18]吴孔文,钟宏,朱维光,冷成彪,苟体忠.云南大红山层状铜矿床成矿流体研究.岩石学报,2008,09:2045-2057.
[19]王新松,毕献武,冷成彪,唐永永,兰江波,齐有强,沈能平.滇西北中甸红山Cu多金属矿床花岗斑岩锆石LA-ICP-MSU-Pb定年及其地质意义.矿物学报,2011,03:315-321.
[20]苟体忠,钟宏,冷成彪,吴孔文.云南中甸地区烂泥塘低温热液型Cu-Au矿床铂族元素(PGE)地球化学特征.矿物学报,2010,03:319-323.
[21]汪玉会,冷成彪,张兴春.新疆叶城县库喀阿孜铅-锌-(铜-钨)多金属矿区中-酸性侵入岩元素地球化学和年代学初步研究[J].矿物岩石地球化学通报,2013,6:736-745.
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