刘春发.赞比亚Chambishi矿区新元古代Roan群沉积作用及其对铜钴成矿的贡献[D].中国地质大学(北京),2019(02).

孟宪刚.辽西医巫闾山北段中生代构造格架及其对金矿形成富集与分布的控制作用[D].中国地质大学（北京）,2003(03).

王安建等著.脉状金矿地质与成因[M].吉林科学技术出版社,1996.

Liu ChunFa,Qing Min,Liu ShuFei,Ding GaoMing,Liu BiZheng,Liu YanBing,Yu Ping.Genesis of sediment‐hosted stratiform Cu–Co deposits of the Zambia Copperbelt: Geochemistry and S–Pb isotopes constraints from the Chambishi deposit[J].Geological Journal,2021.

Key Laboratory of Mineral Resources, Chinese Academy of Sciences, Institute of Geology and Geophysics Chinese Academy of Sciences Beijing China,College of Earth and Planetary Sciences University of Chinese Academy of Sciences Beijing China,Innovation Academy for Earth Science Chinese Academy of Sciences Beijing China,Key Laboratory of Mineral Resources, Chinese Academy of Sciences, Institute of Geology and Geophysics Chinese Academy of Sciences Beijing China,College of Earth and Planetary Sciences University of Chinese Academy of Sciences Beijing China,Innovation Academy for Earth Science Chinese Academy of Sciences Beijing China,Key Laboratory of Mineral Resources, Chinese Academy of Sciences, Institute of Geology and Geophysics Chinese Academy of Sciences Beijing China,College of Earth and Planetary Sciences University of Chinese Academy of Sciences Beijing China,Innovation Academy for Earth Science Chinese Academy of Sciences Beijing China,Earth Science and Engineering, Shandong University of Science and Technology Qingdao China,Key Laboratory of Mineral Resources, Chinese Academy of Sciences, Institute of Geology and Geophysics Chinese Academy of Sciences Beijing China,College of Earth and Planetary Sciences University of Chinese Academy of Sciences Beijing China,Innovation Academy for Earth Science Chinese Academy of Sciences Beijing China,College of Earth and Planetary Sciences University of Chinese Academy of Sciences Beijing China,State Key Laboratory of Lithospheric Evolution, Chinese Academy of Sciences, Institute of Geology and Geophysics Chinese Academy of Sciences Beijing China,Innovation Academy for Earth Science Chinese Academy of Sciences Beijing China,Key Laboratory of Mineral Resources, Chinese Academy of Sciences, Institute of Geology and Geophysics Chinese Academy of Sciences Beijing China,College of Earth and Planetary Sciences University of Chinese Academy of Sciences Beijing China,Innovation Academy for Earth Science Chinese Academy of Sciences Beijing China.Mineralogy and He–Ar isotopic compositions of pyrites in the Paishanlou Au deposit on the northern margin of North China Craton[J].Geological Journal,2020.

Zeng Qingdong,Wang Yongbin,Yang Jinhuii,Guo Yunpeng,Yu Bing,Zhou Lingli,Qiu Haicheng.Spatial–temporal distribution and tectonic setting of gold deposits in the Northern margin gold belt of the North China Craton[J].International Geology Review,2020.

Zhenjun Sun,Zongqi Wang,Henan Yu,Chengyang Wang,Guanghu Liu,Xaingdong Bai.Fluid Inclusions and CHOSPb Isotopes: Implications for the Genesis of the Zhuanshanzi Gold Deposit on the Northern Margin of the North China Craton[J].Resource Geology,2019.

Jun Deng,Qingfei Wang.Gold mineralization in China: Metallogenic provinces, deposit types and tectonic framework[J].Gondwana Research,2016.

Xiao-Hui Zhang,Qing Liu,Ying-Jun Ma,Hui Wang.Geology, fluid inclusions, isotope geochemistry, and geochronology of the Paishanlou shear zone-hosted Gold Deposit, North China Craton[J].Ore Geology Reviews,2005.

Wenjiao Xiao,Brian F. Windley,Jie Hao,Mingguo Zhai.Accretion leading to collision and the Permian Solonker suture, Inner Mongolia, China: Termination of the central Asian orogenic belt[J].Tectonics,2003(6).

Craig J. R. Hart,Richard J. Goldfarb,Yumin Qiu.Gold deposits of the northern margin of the North China Craton: multiple late Paleozoic-Mesozoic mineralizing events[J].Mineralium deposita,2002.

D.I Groves,R.J Goldfarb,M Gebre-Mariam,S.G Hagemann,F Robert.Orogenic gold deposits: A proposed classification in the context of their crustal distribution and relationship to other gold deposit types[J].Ore Geology Reviews,1998(1).

B. N. Eisenlohr,D. Groves,G. A. Partington.Crustal-scale shear zones and their significance to Archaean gold mineralization in Western Australia[J].Mineralium Deposita,1989(1).

Hiroshi Ohmoto.Stable isotope geochemistry of ore deposits[J].1986.

R.E. Zartman,B.R. Doe.Plumbotectonicsa??the model[J].Tectonophysics,1981(1-2).

Veizer Ján,Holser William T,Wilgus Cheryl K.Correlation of 13C12C and 34S32S secular variations[J].Geochimica et Cosmochimica Acta,1980(4).

Deines P.The isotopic composition of carbonatite and kimberlite carbonates and their bearing on the isotopic composition of deep-seated carbon[J].Geochimica et Cosmochimica Acta,1973(7).

韩小梦,郭云成,段留安,王建田,赵鹏飞,王利鹏,喻光明.胶莱盆地东北缘前垂柳金矿床S、Pb同位素组成:对成矿物质来源的指示[J].地质科技通报,2023(03).

罗华,郭盼,刘力,潘龙克,段先锋,毛启曦,廖明芳.湖北来凤革勒车地区铅锌-萤石矿流体包裹体与C-H-O-S-Pb同位素特征及其地质意义[J].地质科技通报,2024(01).

严子清,石文杰,张鹏涛,王勇军,邵玉宝,黄鑫,宋宇,谭俊,王治华.胶东大尹格庄金矿成矿流体时空演化及矿床成因：来自流体包裹体、成矿元素和H-O-S-Pb同位素证据[J].地质科技通报,2024(02).

韩嫣,胡雅婷,王倩,石明辉,周炼.铜同位素及其在环境污染示踪中的应用进展[J].地质科技通报,2023(01).

刘彦兵,屈海浪,胡博心,缪广,滕俊伟,武昌胜,王睿鹏.辽宁排山楼金矿T4矿体Au元素富集规律及其对找矿的指示意义[J].黄金科学技术,2021(03).

王海,祝新友,王京彬,贾德龙,石煜,陈磊,许正繁.四川天宝山铅锌矿成矿物质来源与成矿机制：来自流体包裹体及同位素地球化学制约[J].岩石学报,2021(06).

薄军委,丁正江,宋明春,邱昆峰,孙丰月,纪攀,许虹,张然.胶东辽上金矿床C、O、S、Pb同位素组成及矿床成因[J].岩石矿物学杂志,2021(02).

王银宏,刘家军,张梅,张方方,王康,咸雪辰,郭灵俊.内蒙古阿扎哈达铜铋矿床流体包裹体和碳-氧-硫-铅同位素地球化学研究[J].地学前缘,2020(02).

武昌胜,史志强,刘彦兵.辽宁排山楼金矿区深部成矿预测及靶区验证效果[J].黄金,2019(12).

王庆飞,邓军,赵鹤森,杨林,马麒镒,李华健.造山型金矿研究进展:兼论中国造山型金成矿作用[J].地球科学,2019(06).

刘洪,李光明,黄瀚霄,肖万峰,闫国强,马东方,张海,张红.藏北商旭造山型金矿床成矿物质来源探讨:C、S、Pb同位素证据[J].地质论评,2018(05).

柯坤家,李艳军,牛明伟,刘奔.造山型金矿床成矿作用若干问题研究进展[J].地质科技情报,2018(05).

聂世嘉,杨言辰,韩世炯,张琳,王凤博.辽宁排山楼金矿床黑云母花岗岩成岩时代及地质意义[J].地球科学与环境学报,2017(02).

吴福元,徐义刚,朱日祥,张国伟.克拉通岩石圈减薄与破坏[J].中国科学:地球科学,2014(11).

张静,苏蔷薇,刘学飞,和中华,周云满,李智,赵凯.滇东南老寨湾金矿床地质及同位素特征[J].岩石学报,2014(09).

倪金龙,刘俊来,唐小玲,赵春强,曾庆栋.排山楼金矿韧性剪切带演化过程[J].中国科学:地球科学,2014(07).

孙守恪中国科学院地质与地球物理研究所,刘红涛中国科学院地质与地球物理研究所,褚少雄中国科学院地质与地球物理研究所.辽宁省排山楼矿区二长花岗岩成因及其与金矿化的关系[J].岩石学报,2012(02).

朱日祥,陈凌,吴福元,刘俊来.华北克拉通破坏的时间、范围与机制[J].中国科学:地球科学,2011(05).

赵越,陈斌,张拴宏,刘建民,胡健民,刘健,裴军令.华北克拉通北缘及邻区前燕山期主要地质事件[J].中国地质,2010(04).

张静,杨艳,胡海珠,王志光,李国平,李忠烈.河南银洞沟造山型银矿床碳硫铅同位素地球化学[J].岩石学报,2009(11).

王荣湖,金成洙,李景春.排山楼金矿床~(40)Ar-~(39)Ar年龄及其地质意义[J].东北大学学报(自然科学版),2008(10).

翟明国.华北克拉通中生代破坏前的岩石圈地幔与下地壳[J].岩石学报,2008(10).

殷莉,张瑞生,郑建平.金刚石包裹体矿物化学特征与华北东部克拉通岩石圈地幔属性[J].地质科技情报,2008(05).

张岳桥,董树文.郯庐断裂带中生代构造演化史: 进展与新认识[J].地质通报,2008(09).

陈衍景,倪培,范宏瑞,F Pirajno,赖勇,苏文超,张辉.不同类型热液金矿系统的流体包裹体特征[J].岩石学报,2007(09).

陈衍景.造山型矿床、成矿模式及找矿潜力[J].中国地质,2006(06).

吴福元,杨进辉,张艳斌,柳小明.辽西东南部中生代花岗岩时代[J].岩石学报,2006(02).

李三忠,刘建忠,赵国春,吴福元,韩宗珠,杨中柱.华北克拉通东部地块中生代变形的关键时限及其对构造的制约——以胶辽地区为例[J].岩石学报,2004(03).

刘家军,何明勤,李志明,刘玉平,李朝阳,张乾,杨伟光,杨爱平.云南白秧坪银铜多金属矿集区碳氧同位素组成及其意义[J].矿床地质,2004(01).

毛景文,赫英,丁悌平.胶东金矿形成期间地幔流体参与成矿过程的碳氧氢同位素证据[J].矿床地质,2002(02).

罗镇宽,苗来成,关康,裘有守,Y.M.Qiu,N.J.McNaughton,D.I.Groves.辽宁阜新排山楼金矿区岩浆岩锆石SHRIMP定年及其意义[J].地球化学,2001(05).

李俊建,沈保丰,骆辉,翟安民,曹秀兰,桑海清.辽宁阜新排山楼金矿的~(40)Ar/~(39)Ar成矿年龄[J].地质科学,2001(01).

胡明安,章传玲.四川石棉田湾金矿床韧性剪切构造带地球化学障的成矿意义[J].地质科技情报,2000(02).

骆辉,赵运起.辽宁阜新排山楼金矿地质和成矿作用[J].前寒武纪研究进展,1997(04).

刘建明,刘家军,顾雪祥.沉积盆地中的流体活动及其成矿作用[J].岩石矿物学杂志,1997(04).

吴春林,孙厚江.排山楼地区金矿控制条件分析[J].黄金地质,1996(02).

李达，韩雪梅.排山楼金矿地质特征及成矿模式初探[J].贵金属地质,1995(02).

张耀华,谷振东,陈为民.阜新排山楼金矿金的赋存状态[J].辽宁地质,1993(02).

曲亚军,高殿生,贾云伟,刘贵,白明山,郭宝军,许云鹏.排山楼金矿床的蚀变特征[J].辽宁地质,1992(01).

吴春林.排山楼韧性剪切带型金矿床特征及成矿作用[J].矿产与地质,1991(05).