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[1]XinghaiLang*,JuxingTang,QingYin,ZhiweiCui,YongHuang,JinshuZhang,YimingGao,ZhijunLi,FengDing,FuweiXie,ZongyaoYang,MinZeng.GeochemistryandgenesisofEoceneLamprophyresintheXiongcunporphyrycopper-golddistrict,southernmarginoftheLhasaterrane,Tibet,China.GeochemicalJournal,2017,51(2):123-142
[2]XinghaiLang,JuxingTang*,ZhijunLi,YongHuang,FengDing,HuanhuanYang,FuweiXie,LiZhang,QinWang,YunZhou.U–PbandRe–OsgeochronologicalevidencefortheJurassicporphyrymetallogeniceventoftheXiongcundistrictintheGangdeseporphyrycopperbelt,southernTibet,PRC.JournalofAsianEarthSciences,2014,79(2):608-622
[3]JuxingTang,XinghaiLang*,FuweiXie,YimingGao,ZhijunLi,YongHuang,FengDing,HuanhuanYang,LiZhang,QinWang,YunZhou.GeologicalcharacteristicsandgenesisoftheJurassicNo.IporphyryCu-AudepositintheXiongcundistrict,Gangdeseporphyrycopperbelt,Tibet.OreGeologyReviews,2015,70(4):438-456
[4]XinghaiLang,DongLiu*,YulinDeng,JuxingTang,XuhuiWang,ZongyaoYang,ZhiweiCui,YongxinFeng,QingYin,FuweiXie,YongHuang,JinshuZhang.DetritalzircongeochronologyandgeochemistryofJurassicsandstonesintheXiongcundistrict,southernLhasasubterrane,Tibet,China:implicationsforprovenanceandtectonicsetting.GeologicalMagazine,2018,doi:10.1017/S0016756818000122
[5]XinghaiLang*,JuxingTang,YulinDeng,FuweiXie,ZongyaoYang,ZhiweiCui,XuhuiWang,ZhijunLi,ZhongZhang,JinshuZhang,YongHuang.NewDiscoveryofthe341MaGabbroatXiongcunDistrictintheSouthernMarginofLhasaTerrane,Tibet.ActaGeologicaSinica(EnglishEdition),2018,92(1):420-421
[6]XinghaiLang*,XuhuiWang,JuxingTang,YulinDeng,ZhiweiCui,QingYin,FuweiXie.CompositionandageofJurassicdiabasedikesintheXiongcunporphyrycopper–golddistrict,southernmarginoftheLhasaterrane,Tibet,China:Petrogenesisandtectonicsetting.GeologicalJournal,2017,DOI:10.1002/gj.3028
[7]MinZeng,XiangZhang*,HuiCao,FrankR.Ettensohn,WenbinCheng,XinghaiLang.LateTriassicinitialsubductionoftheBangong-NujiangOceanbeneathQiangtangrevealed:stratigraphicandgeochronologicalevidencefromGaize,Tibet.BasinResearch,2016,28(1):147-157
[8]郎兴海*,唐菊兴,邓煜霖,谢富伟,杨宗耀,崔志伟,王旭辉,李志军,张忠,张金树,黄勇.西藏拉萨地块南缘雄村矿集区首次发现早石炭世辉长岩:古特提斯洋的残留?.地球学报,2017,38(05):745-753
[9]郎兴海*,王旭辉,崔志伟,邓煜霖,谢富伟,尹青.西藏雅鲁藏布江南岸若措早侏罗世含矿斑岩的锆石U-Pb年龄及地质意义.矿物岩石,2017(4):74-87
[10]郎兴海*,崔志伟,王旭辉,邓煜霖,谢富伟,韩鹏,杨宗耀,张忠,黄勇,李志军,尹青,张金树,丁枫,董树义,王子正,张丽.西藏谢通门县雄村矿集区综合信息找矿模型及靶区预测.地球学报,2017,38(05):790-802
[11]郎兴海,唐菊兴*,杨宗耀,丁帅,胡古月,李玉海,谢富伟,严成名.西藏自治区谢通门县斯弄多铅锌矿区地球物理特征及找矿方向.地质与勘探,2017,53(03):508-518
[12]郎兴海,崔志伟*,骆毓燕.我国的固体矿产勘查项目融资方式探讨.国土资源科技管理,2016,33(5):58-64
[13]郎兴海*,唐菊兴,谢富伟,黄勇.西藏雄村矿区地面磁测异常特征及其对找矿方向的指示,地质与勘探,2014,50(3):411-418
[14]郎兴海*,唐菊兴,谢富伟,李志军,黄勇,丁枫,杨欢欢,周云,王勤.西藏雄村矿区南部玢岩的地质年代学、岩石地球化学及其地质意义.大地构造与成矿学,2014,38(3):609-620
[15]郎兴海*,唐菊兴,李志军,董树义,丁枫,谢富伟,王子正,张丽,黄勇.化探在西藏雄村矿区Ⅱ、Ⅲ号矿体发现中的作用.物探与化探,2014,38(4):667-672
[16]郎兴海*,唐菊兴,胡正华,谢富伟,黄勇.西藏雄村矿区Ⅲ#矿体成矿流体特征.金属矿山,2014,32(9):95-98
[17]郎兴海*,唐菊兴,李志军,谢富伟,黄勇.西藏冈底斯斑岩铜矿带雄村矿区侏罗纪成矿作用:来自锆石U-Pb和辉钼矿Re-Os年龄的证据.矿物学报,2013(s2):328-328
[18]郎兴海*,唐菊兴,李志军,董树义,丁枫,王子正,张丽,黄勇.西藏谢通门县雄村铜金矿区及其外围的找矿前景地球化学评价.地质与勘探,2012,48(1):12-23
[19]郎兴海*,唐菊兴,陈毓川,李志军,黄勇,王成辉,陈渊,张丽,周云.西藏冈底斯成矿带南缘新特提斯洋俯冲期成矿作用:来自雄村矿集区Ⅰ号矿体的Re-Os同位素年龄证据.地球科学-中国地质大学学报,2012,37(3):515-525
[20]郎兴海*,唐菊兴,李志军,黄勇,丁枫,王成辉,张丽,周云.西藏雄村斑岩型铜金矿集区Ⅰ号矿体的硫、铅同位素特征及其对成矿物质来源的指示.地球学报,2012,33(4):459-470
[21]郎兴海*,唐菊兴,李志军,黄勇,陈渊,张丽.西藏谢通门县雄村斑岩型铜金矿集区Ⅰ号矿体的蚀变与矿化特征.矿床地质,2011,30(2):327-338
[22]郎兴海*,陈毓川,唐菊兴,李志军,邓起,黄勇,陈渊,张丽.西藏谢通门县雄村斑岩型铜金矿床成因讨论——来自元素的空间分布特征的证据.地质论评,2010,56(3):384-402
[23]郎兴海*,陈毓川,唐菊兴,李志军,黄勇,王成辉,陈渊,张丽.西藏谢通门县雄村斑岩型铜金矿集区Ⅰ号矿体的岩石地球化学特征:对成矿构造背景的约束.地质与勘探,2010,46(5):887-898
[24]郎兴海*,唐菊兴,陈毓川,李志军,黄勇,王成辉,陈渊,张丽.西藏谢通门县雄村斑岩型铜金矿集区Ⅱ号矿体中辉钼矿Re-Os年代学及地质意义.矿物岩石,2010,30(4):55-61
[25]郎兴海*,唐菊兴,王子正.西藏冈底斯中段则莫多拉铜金矿床地质特征及找矿方向.地质与资源,2007,16(1):29-33
[26]王旭辉,郎兴海*,邓煜霖,崔志伟,娄渝明,韩鹏.西藏冈底斯南缘汤白斑状花岗岩锆石U-Pb年代学、地球化学及地质意义.高校地质学报,2018,24(1):59-73
[27]杨宗耀,郎兴海*,唐菊兴,张忠,张金树,高一鸣,黄勇,谢富伟,付燕刚,王勇.西藏雄村铜金矿区侏罗系砂岩地球化学特征:对构造背景的约束.地质学报,2017,91(09):1985-2003
[28]李壮,郎兴海*,丁帅,李海峰,杨宗耀,施硕,王立强,李于海.西藏斯弄多浅成低温热液型银铅锌矿床银的赋存状态研究.地球学报,2017,38(05):687-701
[29]谢富伟,郎兴海*,唐菊兴.西藏雄村矿集区侏罗纪斑岩磷灰石矿物化学特征对新特提斯洋俯冲成矿作用的指示.地球学报,2017,38(05):813-828
[30]杨宗耀,郎兴海*,贺元,孟展,谢富伟,银雪琴.云南子尼铜矿床地质特征及深部找矿前景.金属矿山,2016,(03):107-112
[31]尹青,郎兴海*,唐菊兴,张金树,谢富伟,杨宗耀,李志军,黄勇,白云,付红超.西藏雄村矿区Ⅱ号矿体硫、铅同位素地球化学特征.矿床地质,2015,34(05):1016-1029
[32]丁枫,郎兴海*,胡正华,杨欢欢,王子正,张丽.西藏雄村铜金矿I号矿体赋矿凝灰岩成因探讨:来自岩石地球化学、Sr-Nd-Pb同位素地球化学特征的证据.地球学报,2012,33(4):546-558