[1] 王之田,秦克章,张守林.大型铜矿地质与找矿.北京:冶金工业出版社,1994,162.

[2] 王之田,刘湘培,宋叔和.美国西南部斑岩铜矿.当今世界地球科学动向—中国科学家谈第28届国际地质大学.北京:地质出版社,1990,174-181.

[3] 王玉往,秦克章.VAMSD 矿床系列最基性端员—青海省德尔尼大型铜钴矿床的地质特征和成因类型.矿床地质,1997,16(1):1-10.

[4]  《江西银山铜铅锌金银矿床》编写组.江西银山铜铅锌金银矿床.北京:地质出版社,1996,308.

[5] 宋淑和.火山活动与成矿的一些问题.第二届全国火山岩会议论文集.北京:地质出版社,1993.12-16.

[6] 汪东波.成矿省和成矿作用的演化—查明矿产分布规律和解决某些重大基础地质问题的关键.有色金属矿产与勘查,1993,2(5):257-263.

[7] 李人树.成矿系统分析的理论与实践.北京:地质出版社,1996.262.

[8] 姜福芝,王玉往.白银矿田块状硫化物矿床几个地质问题的新认识.有色金属矿产与勘查,1992,1(3):129-139.

[9] 涂光炽.关于火山岩型矿床若干问题的探讨.第二届全国火山岩会议论文集.北京:地质出版社,1993.6-12.

[10] 秦克章,王之田,潘龙驹.满洲里—新巴尔虎右旗铜、钼、铅、锌、银带成矿条件与斑岩体含矿性评价标志.地质论评,1990,36(6):478-488.

[11] 秦克章,王之田.内蒙古乌奴格吐山斑岩铜钼矿床稀土元素的行为及意义.地质学报,1993,7(2):323-335.

[12] 秦克章.试论大型- 超大型铜矿床的主要控制因素.地学探索,1993,(8):39-45.

[13] 秦克章,王京彬,朱思才,等.可可塔勒铅锌矿床地质地球化学特征与火山热水—对流循环成矿模型.首届有色系统青年地质工作者学术讨论会论文集,北京:冶金工业出版社,1995,13-16.

[14] 梅友松,汪东波,黄浩,等.同位成矿概论.地质与勘探,1995,31(5):3-14.

[15] 程裕淇,陈毓川,趋一鸣,等.再论矿床的成矿系列问题.中国地质科学院院报,1983,(6):1-52.

[16] Arribas A J r,Hedenquist,J W.Ita Ya T. et al.Contemporaneous formation of adjacent porphyry and epithermal Cu-Au deposits over 300 ka in northern Luzon,Philippines.Geology,1995,(23):337-340.

[17] Campbell I H. Lesher,C M. Coad,P.et al.Rare earth element mobility in alteration pipes below massive Cu-Zn sulfide deposits.chemical Geology,1984,45:181-202.

[18] Hedenquist J W,Lowenstern J B.The role of magmas in the formation of hydrothermal ore deposits Nature,1994,(370):519-527.

[19] Lydon J W.Ore deposits models-8:Volcanic massive sulphide deposits.Part Ⅱ:A genetic model Geoscience Canada,1988,15(1):43-66.

[20] Qin K Z.A comparison of subaerial v2lcano-porphyry Au、Ag、Pb、Zu、Cu deposit systematics with VHMS analogues.Proceedings of 9th IA GOD Symposium,1994.533-534.

[21] Qin Kezhang,Wang Zhitian Pan Longju.Magmatism and metallogenic systematics of the Southern Ergun Mo、Cu、Pb、Zn and Ag belt.Inner Mongolia,China.Resource Geology Special Issue,1995,(18):159-169.

[22] Qin K Z,Ishihara S.On the possibility of porphyry copper mineralization in Japanese Islands. International Geology Review,1998(accepted).

[23] Sawkins F J.Metal Deposits in Relation to Plate Tectonics.2nd rev and enlarged.Springer-Verlag 1990.85-110.

[24] Sillitoe R H.Are porphyry copper and Kuroko2type massive sulfide deposits incompatible.Geology,1980,8:11-14.

[25] Sillitoe R H.Enargite2bearing massive sulfide deposits high in porphyry copper systems.Economic Geology,1983,78:348-352.

[26] Thompson J F H ed.Magmas,Fluids,and Ore Deposits.Mineralogical Association of Canada Short-Course 23,1995.525p.

[27] Urabe T.Kuroko deposit modeling based on magmatic hydrothermal theory.Mining Geology,1987,37:159-176.