“上山”找金铜, “下山”找钨锡及其理由

张旗; 金惟俊; 李承东; 王元龙

“上山”找金铜, “下山”找钨锡及其理由

1.
中国科学院地质与地球物理研究所, 北京 100029
2.
中国地质调查局天津地质矿产研究所, 天津 300170

基金项目:

国家自然科学基金重大研究计划 90714011

详细信息

作者简介:
张旗(1937-).男, 研究员,从事岩石学和地球化学研究.E-mail: zhangqi@mail.igcas.ac.cn

中图分类号: P588.12;P618.2
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出版历程
- 收稿日期: 2008-09-02
- 刊出日期: 2009-07-25

Reason for Gold and Copper Discovery in Mountain with Tungsten and Tin Discovery on Plain

1.
Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029
2.
Tianjin Institute of Geology and Mineral Resources, China Geological Survey, Tianjin 300170

摘要

摘要: 金铜和钨锡是两种不同类型的矿产资源, 金铜经常伴生, 钨锡经常伴生, 金铜和钨锡通常不在一起.研究表明, 金铜主要与埃达克岩和喜马拉雅型花岗岩有关, 产于加厚的地壳底部, 地表相应的出现高原或山脉; 钨锡主要与南岭型花岗岩有关, 代表减薄的陆壳, 产于平原区, 地势较低.因此, 从找矿的角度来说, 应当“上山”找金铜, “下山”找钨锡.文中识别出中国三叠纪以来可能存在过的7个山脉(华北北部山脉、西秦岭-东昆仑山脉、额尔古纳山脉、松潘-中甸山脉、湘赣山脉、浙闽山脉和哀牢山-羌塘山脉) 和2个高原(中国东部高原和湖南山地) 以及现存的青藏高原, 建议在上述高原和山脉上去找金铜矿, 指出喜马拉雅型花岗岩与金矿的密切关系, 是今后找金矿的一个重要目标.认为钨锡成矿目前仍然以华南为最佳, 但应注意在其他地块寻找钨锡的问题.
- 高原 /
- 山脉 /
- 平原 /
- 埃达克岩 /
- 南岭型花岗岩 /
- 金铜 /
- 钨锡
Abstract: Gold and copper are two different types of mineral resources.Gold and copper are often accompanied, while tungsten and tin are often accompanied, but gold and copper are usually not together with tungsten and tin.Researches indicate the gold and copper, mainly connected with the adakite and Himalaya-type granite, originated in the thickened bottom of crust.And correspondingly, plateau or the mountain occur on the earth's surface.The tungsten and tin are mainly relevant to the granite from Nanling area of China, and represent the thinned crust originated in the plain area with the relative low elevation.Therfore, from the view of prospecting, the gold and copper should be prospected in a mountain, while the tungsten and tin should be prospected in a plain.In this paper, we suggest that seven mountains in China (such as North Mountain of the North China, West Qinling-East Kunlun mountains, Erguna mountain, Songpan-Zhongdian mountain, Hunan-Jiangxi mountain, Fujian-Zhejiang mountain and the Ailaoshan-Qiangtang mountain), two plateaus (East China Plateau and Hunan Range) and present Qinghai-Xizang Plateau would be the spot where gold and copper can be prospected since the Triassic period in China.We propose to prospect gold and copper ore on these plateaus and mountains, and point out that the gold is closely related to the Himalaya type granite.We believe that the South China is best place to prospect tungsten and tin, but attention should be also paid on prospecting tungsten and tin in other places.
- plateau /
- mountain /
- plain /
- adakite Nanling-type granite /
- gold and copper /
- tungsten and tin /

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图 1 南岭型(典型的A型) 花岗岩的REE (a) 和微量元素蛛网图(b)

REE标准化数值据Taylor and McLennan (1985); 微量元素标准化数值据Sun and McDonough (1989); 数据引自Zhang et al. (2007)

Fig. 1. (a) Chondrite-normalized REE patterns and (b) primitive mantle-normalized element spider diagram for the Nanling-type granites

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图 2 小秦岭埃达克岩与金矿分布图(据罗铭玖等, 2000,修改)

实心圆.金矿; Q.第四系; Pt.元古界蓟县系; Ar.太华群.华山、文峪和娘娘山花岗岩为埃达克岩, 金矿赋存于古老变质岩系中, 但其成因与埃达克岩有关

Fig. 2. Distribution of adakites and gold depoeits in the Xiaoqinling area

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图 3 与金、铜、钨、锡有关的花岗岩的Sr-Yb图

金矿: 冀北中生代花岗岩(包括大石镐、肖营子、小庙沟、高家店、马道沟、贾家山、都山、柏仗子、大野峪、红花梁、响水沟、谷咀子、上水泉、青山口、峪耳崖和牛心山等), 据李承东等, 2004; 小秦岭(包括文峪、娘娘山、华山、老牛山), 据罗铭玖等, 2000,; 铜矿(作者注: 著名的斑岩铜矿如德兴、长江中下游、玉龙和冈底斯等已经有了许多报道, 此处就不重复了, 仅列举与本文有关的若干资料) : 湘东北金井(李鹏春等, 2005); 湘东北赤马和石蛤蟆(彭头平等, 2004); 湖南水口山(马丽艳等, 2006); 福建紫金山(赵希林, 2007); 钨锡矿: 南岭(陈富文和付建明, 2005); 湖南锡田(马铁球等, 2004; 余阳春等, 2006); 黄沙坪(姚军明等, 2005); 王仙岭(柏道远等, 2007b); 骑田岭(汪雄武等, 2004; 邓希光等, 2005; 付建明等, 2006); 广西大厂和芒场(蔡明海等, 2004a, 2004b); 西藏申扎嘎若(王治华等, 2006).图中红色虚线圈定的是华北北部与金矿有关的花岗岩分布范围(据李承东等, 2004); 绿色实线圈定的为华南与金铜有关的花岗岩; 紫色实线圈定的为华南与钨锡有关的花岗岩

Fig. 3. Sr-Yb diagram related to granites with gold-, copper-, tungsten- and tin deposits, respectively

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图 4 不同类型花岗岩和钨、锡、金、铜成岩成矿模式

图中主要说明不同类型的花岗岩和不同类型成矿的深度不同: 埃达克岩形成的深度最深, 有利于金铜的萃取; 喜马拉雅型花岗岩形成的深度较深, 有利于金的萃取; 南岭型花岗岩形成的深度最浅, 有利于钨锡的萃取.图中假定岩浆和矿液的萃取是在下地壳底部发生的, 钨锡主要来自下地壳, 金铜既可来自下地壳, 也可来自底侵的玄武岩

Fig. 4. Model for distinct granite types with tungsten-, tin-, gold-, and copper deposits mineralization, respectively

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图 5 中国三叠纪以来高原和山脉分布

星号.埃达克岩(实心-侵入岩; 空心-喷出岩), 不同时代的埃达克岩用颜色予以区分: 蓝色.三叠纪-早侏罗世; 绿色.侏罗纪; 红色.白垩纪; 黄色.第三纪; 实心方块.喜马拉雅型; 蓝色粗点线示高原; 绿色粗虚线示山脉; 红色粗实线示今后找矿的重点区.湖南山地范围内花岗岩的分布见图 6.本图未表示中国东部高原和青藏高原范围内埃达克岩和喜马拉雅型花岗岩的分布, 详见张旗等(2008c, 2008d)

Fig. 5. Distribution map on plateaus and mountains in Mesozoic periods in China

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图 6 湖南山地不同类型花岗岩和金等资源分布

实心方块.喜马拉雅型花岗岩; 五角星.埃达克岩; 菱形.浙闽型花岗岩; 三角形.南岭型花岗岩; 阴影实心圆.金矿; 黑色实心圆.铜矿; 实线.以岩石资料圈定的湖南山地范围; 虚线.以岩石和金铜矿床资料重新圈定的湖南山地范围.岩石资料据贾大成等, 2003; 徐夕生等, 203;伍光英等, 2005; 王岳军等, 2005, 2007;张敏等, 2006;柏道远等, 2007;Wanget al 2006., .矿床资料据彭渤和黄瑞华, 1996; 康如华等, 2001; 李福顺等, 2002; 赵建光等, 2004; 方向阳等, 2005; 谢新泉和张衡龙, 2005

Fig. 6. Distribution of variation granite-types and gold-copper deposits in Hunan Hill

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图 7 浙闽山脉埃达克岩和金矿分布

实心五星.埃达克质侵入岩; 空心五星.埃达克质火山岩; 阴影实心圆.金矿.资料来源: 周乐尧和邱郁双, 1997; 黄仁生等, 1999; 黄美, 2003; 卢克标, 2004; 毛建仁等, 2004; 陈荣等, 2005

Fig. 7. Distribution of adakites and gold-deposits in Zhejiang-Fujian Mountains

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图 8 华南不同时代山脉和山地分布

a.综合示意图; b.三叠纪的湖南山地; c.中侏罗世的湘赣山脉; d.晚侏罗世的滇桂湘赣闽粤低地(黑色实心圆示钨锡矿床); e.早白垩世的浙闽山脉.箭头示构造挤压方向

Fig. 8. Distribution map of mountains and hills for distinct periods

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表 1 花岗岩Sr-Yb分类

Table 1. Classification of granites based on Sr and Yb contents

参考文献(200)

Atherton, M. P., Petford, N., 1993. Generation of sodium-rich magmas from newly underplated basaltic crust. Nature, 362: 144-146.
Bai, D. Y., Jia, B. H., Li, J. D., et al., 2007a. Important sig-nificance of regional tectonic regi me to metallogenic ca-pacity of Indosinian and Early Yanshanian granites in southeastern Hunan: A case study of Qianlishan and Wangxianling plutons. Mineral Deposits, 26 (5): 487-500 (in Chinese with English abstract).
Bai, D. Y., Jia, B. H., Ma, T. Q., et al., 2007b. Relationship of petro-geochemical characteristics to metallogenic capacity differences between Indosinian and Early Yans-hanian granites in southeastern Hunan. Acta Petrologica et Minerologica, 26 (5): 387-398 (in Chinese withEnglish abstract).
Bonin, B., 1990. From orogenic to anorogenic settings: Evo-lution of granitoid suites after a major orogenesis. Geol. J., 25: 261-270.
Cai, M. H., Liang, T., Wu, D. C., et al., 2004a. Geochemical characteristics of granites and its structural genetic en-vironment in the Nandan-Hechi metallogenetic belt, Northwest Guangxi. Geotectonica et Metallogenia, 28 (2): 306-313 (in Chinese with English abstract).
Cai, M. H., Liang, T., Wu, D. C., et al., 2004b. Geochemical characteristics of granites and their tectonic setting of Dachang ore field in Guangxi. Geological Science and Technology Information, 23 (2): 57-62 (in Chinesewith English abstract).
Chen, F. W., Fu, J. M., 2005. Geologica and petrochemica characteristics of main Mesozoic tin-mineralized granit-oids and regional metallogenetic regularities in Nanling region. Geology and Mineral Resources of South China, (2): 12-21 (in Chinese with English abstract).
Chen, P. J., 1997. Coastal mountains of SE China, desertiza-tion and saliniferous lakes of Central China during theUpper Cretaceous. Journal of Stratigraphy, 21 (3): 203-212 (in Chinese with English abstract).
Chen, R., Xing, G. F., Yang, Z. L., et al., 2005. Study on Be-izhang and Lianglong granites and their dark enclaves. Geological Journal of China Universities, 11 (2): 264-275 (in Chinese with English abstract).
Chen, Z. G., Zhang, L. C., Wan, B., et al., 2008. Geochemistry and geological significances of ore-forming porphyry with low Sr and Yb value in Wunugetushan copper-molybdenum deposit, Inner Mongolia. Acta Petrologica Sinica, 24 (1): 115-128 (in Chinese with English abstract).
Chen, Z. G., Zhang, L. C., Zhou, X. H., et al., 2006. Geo-chronology and geochemical characteristics of volcanic rocks section in Manzhouli Xinyouqi, Inner Mongolia. Acta Petrologica Sinica, 22: 2971-2986 (in Chinesewith English abstract).
Collins, W. J., Beams, S. D., White, A. J. R., et al., 1982. Nature and origin of A-type granites with particular ref-erence to southeastern Australia. Contr. Miner. Petrol., 10 (2): 189-200.
Defant, M. J., Drummond, M. S., 1990. Derivation of some modern arc magmas by melting of young subduction lithos phere. Nature, 347: 662-665.
Defant, M. J., Xu, J. F., Kepezhinskas, P., et al., 2002. Ada-kites: Some variations on a theme. Acta Petrologica Sinica, 18 (2): 129-142.
Deng, X. G., Li, X. H., Liu, Y. M., et al., 2005. Geochemical characteristics of Qitianling granites and their implica-tions for mineralization. Acta Petrlogica et Mineralogi-ca, 24 (2): 93-102 (in Chinese with English abstract).
Eby, G. N., 1992. Chemical subdivision of the A-type granit-oids: Petrogenetic and tectonic implications. Geology, 20 (7): 641-644.
Fang, X. Y., Dai, P. Y., Wu, S. H., 2005. Analysis of the metallogenetic conditions of Tangfuping gold field in Yuanling County, Hunan Province. Geology and Miner-al Resources of South China, (1): 41-46 (in Chinesewith English abstract).
Feeley, T. C., Davidson, J. P., 1994. Petrology of calc-alka-line lavas at Volcan Ollague and the origin of composi-tional diversity at Central Andean Stratovolcanoes. Journal Petrology, 35: 1295-1340.
Fu, J. M., Xie, C. F., Peng, S. B., et al., 2006. Geochemistry and crust-mantle magmatic mixing of the Qitianling granites and their dark microgranular enclaves in HunanProvince. Acta Geoscientica Sinica, 27 (6): 557-569 (inChinese with English abstract).
Ge, W. C., Wu, F. Y., Zhou, C. Y., et al., 2007. Porphyry Cu-Mo deposits in the eastern Xing'an-Mongolian oro-genic belt: Mineralization ages and their geodynamic im-plications Chinese Science Bulletin, 52 (24): 3416-3427.
Green, T. H., 1982. Anatexis of mafic crust and high pres-sure crystallization of andesite. In: Thorpe, R. S., ed., Andesites. John Wiley and Sons, NewJersey, 465-487.
Gu, S. Y., Hua, R. M., Qi, H. W., 2007. A genetic study ofXinlu-Shuiyanba W-Sn orefield, Northeast Guangxi. Mineral Deposits, 26 (3): 265-276 (in Chinese withEnglish abstract).
Hof mann, A. W., 1988. Chemical differentiation of the earth—The relationship between mantle, continental crust, and oceanic crust. Earth and Planetary ScienceLetters, 90 (3): 297-314.
Huang, M., 2003. Geological characteristics of mineralization in the Huangfu area of Jianning County, Fujian Province. Geology of Fujian, 22 (3): 131-139 (in Chinesewith English abstract).
Huang, R. S., Qiu, S. A., Li, Z. S., et al., 1999. Discussion on the characteristics and genesis of the Xiaoban gold deposit of the ductile-shear-zone type in Fujian Province. Geology of Fujian, 18 (4): 178-188 (in Chinesewith English abstract).
Jia, D. C., Hu, R. Z., Zhao, H. J., et al., 2003. Lithogeo-chemical characteristics of the Mesozoic granitic intrusion from the Wangxiang area in northeastern Hunan Province and its tectonic setting. Acta Geologica Sini-ca, 77: 98-103 (in Chinese with English abstract).
Jiang, S. Y., Zhao, K. D., Jiang, Y. H., et al., 2006. New type of tin mineralization related to granite in South China: Evidence from mineral chemistry, element and isotope geochemistry. Acta Petrologica Sinica, 22 (10): 2509-2516 (in Chinese with English abstract).
Jin, C. W., Harris, N. B. W., Xu, R. H., et al., 1990. Pluton-ic rocks of the 1985 Tibet geotraverse, Laasa to Gol-mud. In: Geological evolution of Tibet plateau. Science Press, Beijing, 141-173.
Jin, W. J., Zhang, Q., He, D. F., et al., 2005. SHRIMP dating of adakites in western Qinling and their implications. Acta Petrologica Sinica, 21 (3): 959-966 (inChinese with English abstract).
Kang, R. H., 2001. Orecontrolling characteristics of the Diaoshuidong micro-grain disseminated type of gold deposit in Hunan Province. Geology and Resources, 10 (4): 210-214 (in Chinese with English abstract).
Kay, R. W., Kay, S. M., 2002. Andean adakites: Three waysto make them. Acta Petrologica Sinica, 18 (3): 303-311.
Leng, C. B., Zhang, X. C., Chen, Y. J., et al., 2007. Discussion on the relationship between Chinese porphyry copper deposits and adakitic rocks. Earth Science Frontiers, 14 (5): 199-210 (in Chinese with English abstract).
Li, C. D., Zhang, Q., Miao, L. C., et al., 2004. Mesozoichigh-Sr, low-Y and low-Sr, low-Y types granitoids inthe northern Hebei Province: Geochemistry and petro-genesis and its relation to mineralization of gold depos-its. Acta Petrologica Sinica, 20 (2): 269-284 (in Chi-nese with English abstract).
Li, F. S., Kang, R. H., Chen, Y. W., et al., 2002. The metal-logenic geological condition of Gaojia ao, Hunan Province and its ore-prospecting orientation. Gold, 22 (5): 1-3 (in Chinese with English abstract).
Li, H. X., 1995. Relations with gold and genetic types of the granites in Hunan Province. Journal of Precious Me-tallic Geology, 4: 283-293.
Li, M., Zhang, C. L., Fan, K. Z., et al., 2004. Geochemical characteristics of Miba intrusion in the South Qinling belt and its geological significance. Journal of North-west University (Natural Science Edition), 34 (3): 325-330 (in Chinese with English abstract).
Li, P. C., Xu, D. R., Chen, G. H., et al., 2005. Constraints of petrography, geochemistry and Sr-Nd isotopes on theJinjing granitoids from northeastern Hunan Province. Acta Petrologica Sinica, 21 (3): 921-934 (in Chinesewith English abstract).
Liu, H. T., Zhang, Q., Liu, J. M., et al., 2004. Adakite versur porphyry copper and epithermal gold deposits: A possible metallogenetic specialization of magmatism required in-deep assessment. Acta Petrologica Sinica, 20 (2): 205-218 (in Chinese with English abstract).
Lu, K. B., 2004. Geologic and geochemical characteristics of the Jiankeng gold deposit in Jian'ou County, Fujian Province and its forecast and appraisement. Geology of Fujian, 23 (2): 104-109 (in Chinese with English abstract).
Lü, Y. F., 1997. Genesis characteristics of Mesozoic granitoid in South Liaoning (Zhuanghe-Dandong) and its relation with gold deposits. Liaoning Geology, (4): 292-302 (in Chinese with English abstract).
Luo, M. J., Li, S. M., Lu, X. X., et al., 2000. Metallogenesis and deposit series of main mineral resources of Henan Province. Geological Publishing House, Beijing, 1-355 (in Chinese).
Ma, L. Y., Lu, Y. F., Mei, Y. P., et al., 2006. ZirconSHRI MP U-Pb dating of granodiorite from Shuikoush-an ore-field, Hunan Province and its geological signifi-cance. Acta Petrologica Sinica, 22 (10): 2475-2482 (inChinese with English abstract).
Ma, T. Q., Wang, X. H., Bai, D. Y., 2004. Geochemical characteristics and its tectonic setting of the Xitian tungsten-tin-bearing granite pluton. Geology and Mi-naral Resources of South China, (1): 11-16 (in Chi-nese with English abstract).
Mao, J. R., Xu, N. Z., Hu, Q., et al., 2004. The Mesozoicrock-forming and ore-forming processes and tectonicenvironment evolution in Shanghang-Datian region, Fujian. Acta Petrologica Sinica, 20 (2): 285-296 (inChinese with English abstract).
Mao, J. W., Xie, G. Q., Zhang, Z. H., et al., 2005. Mesozoiclarge scale metallogenic pulses in North China and cor-responding geodynamic settings. Acta Petrologica Sinica, 21: 169-188 (in Chinese with English abstract).
Martin, H., 1999. Adakitic magmas: Modern analogues of Archean granitoids. Lithos, 46: 411-429.
Oyarzun, R., Mórquez, A., Lillo, J., et al., 2001. Giant ver-sus small porphyry copper deposits of Cenozoic age innorthern Chile: Adakitic versus normal calc-alkaline magmatism. Mineral Deposit, 36: 794-798.
Pati o Douce, A. E., 1999. What do experi ments tell us aboutthe relative contributions of crust and mantle to the ori-gin of granitic magmas?In: Castro, A., Fernandez, C., Vigneresse, J. L., eds. Understanding granite: Integra-ting new and classical techniques. Geological Society, London, Special Publications, 158: 55-75.
Patino Douce, A. E., 1997. Generation of metaluminous A-type granites by low-pressure melting of calc-alkalinegranitoids. Geology, 25 (8): 743-746.
Peng, B., Huang, R. H., 1996. Tectonic-metallogenetic study on ore-finding perspective of rock-gold ore deposits in Hunan Province. Geology-Geochemistry, (1): 56-60 (in Chinese).
Peng, T. P., Xi, X, W., Wang, Y. J., et al., 2004. Geochemical characteristics of the Early Mesozoic granodiorites and their tectonic implications. Geotectonica et Metallo-genia, 28 (3): 287-296 (in Chinese with English ab-stract).
Qian, C. C., Lu, Y. L., Liu, L. L., 2004. Geochemical caractristics and genesis of Yanshannian granite in the Dabie ultra-high-pressure (UHP) metamorphic belt Geology in China, 31 (2): 147-154 (in Chinese with English abstract).
Qin, K. Z., Li, H. M., Li, W. J., et al., 1999. Intrusion and mineralization ages of the Wunugetushan porphyry CuMo deposit, Inner Mongolia, northwestern China. Geological Review, 45 (2): 180-185 (in Chinese with Eng-lish abstract).
Rui, Z, Y., Hou, Z. Q., Li, G. M., et al., 2006. Subduction, collision, deep fracture, adakite and porphyry copper deposits. Geology and Prospecting, 42 (1): 1-6 (inChinese with English abstract).
Sajona, F. G., Maury, R. C., 1998. Association of adakiteswith gold and copper mineralization in the Philippines. CR ACAD SCI II A, 326 (1): 27-34.
Sui, Z. M., Ge, W. C., Wu, F. Y., et al., 2007. Zircon U-Pb ages, geochemistry and its petrogenesis of Jurassic granites in northeastern part of the Da Hinggan Mts. Acta Petrologica Sinica, 23: 461-480 (in Chinesewith English abstract).
Sun, S. S., McDonough, W. F., 1989. Chemical and isotopicsystematics of oceanic basalts: Implications for mantlecomposition and processes. In: Saunders, A. D., Norry, M. J., eds., Magmatismin the ocean basins. GeologicalSociety of London Special Publication, 42: 313-345.
Sylvester, P. J., 1989. Post-collisional alkaline granites. Journal of Geology, 97: 261-280.
Tan, J., Wei, J. H., Li, Y. J., et al., 2007. Some reviews on dia-genesis and metallogeny of the Mesozoic crustal remeltinggranitoids in the Nanling region. Geology Review, 53 (3): 349-362 (in Chinese with English abstract).
Taylor, S. R., McLennan, S. M., 1985. The continental crust: Its composition and evolution, an examination of the geochemical record preserved in sedimentary rocks. Blackwell Science Publisher, Oxford, UK.
Thiéblemont, D., Stein, G., Lescuyer, J. L., 1997. Gisementsépithermaux et porphyriques: La connexion adakite. Earth Planet. Sci., 325 (2): 103-109.
Wang, X. W., Wang, X. D., 2001. Geochemical signs of mineralized granite. Geology and Mineral Resources of South China, (4): 36-44 (in Chinese with English ab-stract).
Wang, X. W., Wang, X. D., Liu, J. Q., et al., 2004. Relationship of Qitianling granite to Sn mineralizationin Hunan Province. Geological Science and Technology Information, 23 (2): 1-12 (in Chinese with English abstract).
Wang, X. Y., Zhao, C. R., Wang, Z. Y., et al., 2004. Indus-trial types and geological features of the northernDaxing anling gold deposits. Gold Geology, 10 (2): 50-54 (in Chinese with English abstract).
Wang, Y., 2002. On the geodynamic significance of strongly peraluminous granitoids of Yanshanian period in the eastern part of China-Case studies on the Hebei-Shanxi-Liaoning area and the Wuchuan-Sihui area of Guangdong. Beijing Geology, 14 (3): 1-10 (in Chinesewith English abstract).
Wang, Y., 2009. Geochemistry of the Baicha A-type granite in Beijing Municipality: Petrogenetic and tectonic implications. Acta Petrologica Sinica, 25 (1): 13-24 (inChinese with English abstract).
Wang, Y. J., Fan, W. M., Liang, X. Q., et al., 2005. SHRIMP zircon U-Pb geochronology of Indosinian granites in Hunan Province and its petrogenetic implications. Chinese Science Bulletin, 50: 1395-1403.
Wang, Y. J., Fan, W. M., Sun, M., et al., 2007. Geochrono-logical, geochemical and geothermal constraints on petrogenesis of the Indosinian peraluminous granites in the South China block: Acase studyinthe Hunan Province. Lithos, 96 (3-4): 475-502.
Wang, Y. T., Mao, J. W., Lu, X. X., et al., 2002. ⁴⁰Ar-³⁹Ar-dating and geological implication of auriferous altered rocks from the middle-deep section of Q875 gold-quartz vein in Xiaoqinling area, Henan, China. Chinese Science Bulletin, 47: 1750-1755.
Wang, Z. H., Wu, X. Q., Wang, K. Q., et al., 2006. Geochemical characteristics of the Garuo monzogranite in the Jaggang Xueshan W-Mo (-Bi) district, southwestern Xainza, Tibet, China. Geological Bulletin of China, 25 (12): 1487-1491 (in Chinese with English abstract).
Wei, C. S., Zheng, Y. F., Zhao, Z. F., 2001. Nd-Sr-O isotopic geochemistry constraints on the age and origin of the A-type granites in eastern China. Acta Petrologica Sini-ca, 17 (1): 95-111 (in Chinese with English abstract).
Wei, J. Q., Zhan, M. G., Lu, Y. F., et al., 1997. Geochemistry of granitoids in Yangla ore district, western Yunnan. Geology and Mineral Resources of South China, (4): 50-56 (in Chinese with English abstract).
Whalen, J. B., Currie, K. L., Chappell, B. W., 1987. A-type granites: Geochemical characteristics, discriminations and petrogenesis. Contributions to Mineralogy and Pe-trology, 95 (4): 407-419.
Wu, G., Chen, Y. J., Sun, F. Y., et al., 2008. Geochemistry of the Late Jurassic graniitoids in the northern end area of Da Hinggan Mountains and their geological and prospecting implications. Acta Petrologica Sinica, 24: 899-910 (in Chinese with English abstract).
Wu, G. Y., Pan, Z. F., Li, J. D., et al., 2005. Geological and geochemical characteristics of the Dayishan granitoids in southern Hunan and their relations to mineralization. Chinese Geology, 32 (3): 434-442 (in Chinese withEnglish abstract).
Xiao, L., Zhang, H. F., Clemens, J. D., et al., 2007. Late Triassic granitoids of the eastern margin of the Tibetan plateau: Geochronology, petrogenesis and implicationsfor tectonic evolution. Lithos, 96 (3-4): 436-452.
Xie, C. F., Zhu, J. C., Ding, S. J., et al., 2006. Age and petrogenesis of the Jianfengling granite and its relationship to metallogenesis of the Baolun gold deposit, Hannan Island. Acta Petrologica Sinica, 22 (10): 2493-2508 (in Chinese with English abstract).
Xie, X. Q., Zhang, H. L., 2005. Geological characteristics and genesis of the Jinshui copper deposit in Chengbu County, Hunan Province. Geology and Mineral Resources ofSouth China, (1): 37-40 (in Chinese with English ab-stract).
Xiong, X. L., Li, X. H., Xu, J. F., et al., 2003. Extremely high-Na adakite-like magmas derived from alkali-rich basaltic underplate: The Late Cretaceous Zhantang andesites in the Huichang basin, SE China. Geochemical Journal, 37 (2): 233-252.
Xu, Q. D., Zhong, Z. Q., Zhou, H. W., et al., 1998. ⁴⁰Ar/39Ar dating of the Xiaoqinling gold area in Henan Province. Geology Review, 44: 323-327 (in Chinese withEnglish abstract).
Xu, X. S., Deng, P., O Reilly, S. Y. O., et al., 2003. Single zircon LAM-ICPMS U-Pb dating of Guidong complex (SE China) and its petrogenetic significance. ChineseScience Bulletin, 48 (17): 1892-1899.
Yang, J. H., Wu, F. Y., Chung, S. L., et al., 2006. A hybrid origin for the Qianshan A-type granite, Northeast China: Geochemical and Sr-Nd-Hf isotopic evidence. Lithos, 89 (1-2): 89-106.
Yang, J. H., Zhu, M. F., Liu, W., et al., 2003. Geochemistry and petrogenesis of Guojialing granodiorites from the northwestern Jiaodong Peninsula, eastern China. ActaPetrologica Sinica, 19: 692-700 (in Chinese with Eng-lish abstract).
Yao, J. M., Hua, R. M., Lin, J. F., 2005. Zircon LA-ICPMSU-Pb dating and geochemical characteristics of Huang-shaping granite in Southeast Hunan Province, China. Acta Petrologica Sinica, 21 (3): 688-696 (in Chinesewith English abstract).
Ye, H. S., Mao, J. W., Li, Y. F., et al., 2006. SHRI MP zir-con U-Pb and molybdenite Re-Os dating for the super-large Donggou porphyry Mo deposit in East Qinling, China, and its geological implication. Acta GeologicaSinica, 80 (7): 1078-1088 (in Chinese with English ab-stract).
Yong, Y. Y., 2007. Tin and tungsten: potential dominant mineral species in the Gangdise belt, Xizang. Sedimentary Geology and Tethyan Geology, 27 (1): 1-8 (inChinese with English abstract).
Yu, Y. G., Wu, S. C., Liang, T. G., 2006. Metallogenetic geological characteristics and ore prospecting direction in Xitian area. Resources Survey and Environment, 27 (2): 136-142 (in Chinese with English abstract).
Zeng, P. S., Li, W. C., Wang, H. P., et al., 2006. The Indosinian Pulang superlarge porphyry copper deposit in Yunnan, China: Petrology and chronology. Acta Petro-logica Sinica, 22 (4): 989-1000 (in Chinese with Eng-lish abstract).
Zhan, F. Y., Gu, F. B., Li, D. S., et al., 2007. Tectonic environment of adakite in eastern Kunlun Area, Qinghai, and its ore-forming significance. Acta Geologica Sinica, 81 (10): 1352-1368 (in Chinese with English ab-stract).
Zhang, C. L., Luo, J. L., Li, M., et al., 2002. Geochemical characteristics and geological significance of Xiba granite, porphyry and porphyrite in East Qinling Journal ofNorthwestern University (Nature science adition), 32 (4): 384-388 (in Chinese with English abstract).
Zhang, H. F., Jin, L. L., Zhang, L., et al., 2005. Geochemical and Pb-Sr-Nd isotopic compositions of granitoids from western Qinling belt: Constraints on basement natureand tectonic affinity. Science in China (Ser. D), 35 (10): 914-926 (in Chinese).
Zhang, H. F., Xiao, L., Zhang, L., et al., 2007. Geochemical and Pb-Sr-Nd isotopic compositions of Indosinian granitoids from the Bikou block, northwest of the Yangtze plate: Constraints on petrogenesis, nature of deep crust and geodynamics. Science in China (Ser. D), 50 (7): 972-983.
Zhang, H. F., Zhang, B. R., Harris, N., et al., 2006. U-Pb zircon SHRIM Pages, geochemical and Sr-Nd-Pb isotopic compositions of intrusive rocks from the Longshan-Tianshui area in the southeast corner of the Qilian orogenic belt, China: Constraints on petrogenesis and tectonic affinity. Journal of Asian Earth Sciences, 27 (6): 751-764.
Zhang, J. J., Chen, Z. H., Wang, D. H., et al., 2008. Geolog-ical characteristics and metallogenic epoch of theXingluokeng tungsten deposit, Fujian Province. Geotectonicaet Metallogenia, 32 (1): 92-97 (in Chinese withEnglish abstract).
Zhang, M., Chen, P. R., Huang, G. L., et al., 2006. The research on the geochemical characteristics of Longyuanba composite pluton in Nanling region. Uranium Geology, 22 (6): 336-344 (in Chinese with English abstract).
Zhang, Q., Pan, G. Q., Li, C. D., et al., 2007. Does fractional crystallization occur in granitic magma?-some crucial questions on granite study (2). Acta Petrologica Sinica, 23: 1239-1251 (in Chinese with English abstract).
Zhang, Q., Qian, Q., Wang, E. Q., et al., 2001. An East China plateau in mid-late Yanshanian period: Implication from adakites. Chinese Journal of Geology, 36 (2): 248-255 (in Chinese with English abstract).
Zhang, Q., Qin, K. Z., Wang, Y. L., et al., 2004. Study on adakite broadened to challenge the Cu and Au explora-tion in China. Acta Petrologica Sinica, 20: 195-204 (in Chinese with English abstract).
Zhang, Q., Wang, Y., Li, C. D., et al., 2006. Granite classification on the basis of Yb and Sr contents and its implications. Acta Petrologica Sinica, 22 (9): 2249-2269 (in Chinese with English abstract).
Zhang, Q., Wang, Y. L., Zhang, F. Q., et al., 2002. Adakite and porphyry copper deposit. Geology and Mineral Re-sources of South China, (3): 85-90 (in Chinese withEnglish abstract).
Zhang, Q., Wang, Y. L., Jin, W. J., et al., 2008a. On the criteria to pre-, syn- and post-orogenic granitic rocks. Geological Bulletin of China, 27 (1): 1-18 (in Chinesewith English abstract).
Zhang, Q., Wang, Y., Jin, W. J., et al., 2008b. Granitic rocks constraint on the Early Mesozoic North Mountain Range in the North China. Geological Bulletin of China, 27 (9): 1391-1403 (in Chinese with English ab-stract).
Zhang, Q., Wang, Y. L., Jin, W. J., et al., 2008c. Late Mesozoic East China plateau: Evidence, remained problemsand implication. Geological Bulletin of China, 27 (9): 1404-1430 (in Chinese with English abstract).
[b289]	Zhang, Q., Wang, Y., Xiong, X. L., et al., 2008d. Adakite and Granite: Challenge and Opportunity. China Land Press, Beijing (in Chinese).
Zhang, T., Zhang, Y. Q., 2007. Geochronological sequence of Mesozoic intrusive magmatism in Jiaodong peninsula and its tectonic constraints. Geological Journal of China Universities, 13 (2): 323-336 (in Chinese with Eng-lish abstract).
Zhao, G. T., Cao, Q. C., Wang, D. Z., et al., 1997. Zirconic U-Pb dating on the Laoshan granitoids and its significance. Journal of Ocean University of Qingdao, 27: 382-388 (in Chinese with English abstract).
Zhao, J. G., Tang, W. G., Xie, Z. H., 2004. Characteristics of geochemical abnormal and its indication effect in Xuefeng gold ore field, Hunan Province. Gold, 25: 11-14 (in Chinese with English abstract).
Zhao, S. Y., Han, Y. D., Zhu, C. L., et al., 2004. Geochemical characteristics and geological significance of interme-diate and intermediate-acid volcanic rocks in the north-ern sector of the Da Hinggan volcanic eruption zone. Journal of Geomechanics, 10: 276-287 (in Chinesewith English abstract).
Zhao, X. L., 2007. The Geochronology Petrography and Geochemical Characteristics of Mesozoic Granitoids from Shanghang Area in SW Fujian and Their Implications (Dissertation). Chinese Acadamy of GeologicalSciences, Beijing.
Zhao, Z. H., Wang, Q., Xiong, X. L., et al., 2006. Two types of adakites in North Xinjiang, China. Acta PetrologicaSinica, 22 (5): 1249-1265 (in Chinese with English ab-stract).
Zhou, L. Y., Qiu, Y. S., 1997. Metallogenic system of gold deposits in Mesozoic continental margin volcanic rocks, Zhejiang. Geologyof Zhejiang, 13 (2): 11-21 (in Chi-nese with English abstract).
Zhu, H. C., Zhang, J. F., Quan, H., 2005. Two stages of Mesozoic lithogenesis and mineralization in Daxing'anling Mountains. Journal of Jilin University (Earth Science Edition), 35: 436-442 (in Chinese withEnglish abstract).
Zorin, Y. A., 1999. Geodynamics of the western part of the Mongolia-Okhotsk collisional belt, Trans-Baikal region (Russia) and Mongolia. Tectonophysics, 306 (1): 33-56.
Zorin, Y. A., Zorina, L. D., Spiridonov, A. M., et al., 2001. Geodynamic setting of gold deposits in eastern and Central Trans-Baikal (Chita Region, Russia). Ore Geology Reviews, 17: 215-232.
柏道远, 贾宝华, 李金冬, 等, 2007a. 区域构造体制对湘东南印支期与燕山早期花岗岩成矿能力的重要意义——以千里山岩体和王仙岭岩体为例. 矿床地质, 26 (5): 487-500. https://www.cnki.com.cn/Article/CJFDTOTAL-KCDZ200705002.htm
柏道远, 贾宝华, 马铁球, 等, 2007b. 湘东南印支期与燕山早期花岗岩成矿能力差异与岩石地球化学特征关系探讨. 岩石矿物学杂志, 26 (5): 387-398. https://www.cnki.com.cn/Article/CJFDTOTAL-YSKW200705002.htm
蔡明海, 梁婷, 吴德成, 等, 2004a. 广西大厂矿田花岗岩地球化学特征及其构造环境. 地质科技情报, 23 (2): 57-62. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ200402013.htm
蔡明海, 梁婷, 吴德成, 等, 2004b. 桂西北丹池成矿带花岗岩地球化学特征及其构造环境. 大地构造与成矿学, 28 (3): 306-313. https://www.cnki.com.cn/Article/CJFDTOTAL-DGYK200403010.htm
蔡明海, 梁婷, 吴德成, 等, 2004b. 桂西北丹池成矿带花岗岩地球化学特征及其构造环境. 大地构造与成矿学, 28 (3): 306-313.
陈丕基, 1997. 晚白垩世中国东南沿岸山系与中南地区的沙漠和盐湖化. 地层学杂志, 21 (3): 203-212. https://www.cnki.com.cn/Article/CJFDTOTAL-DCXZ703.003.htm
陈荣, 邢光福, 杨祝良, 等, 2005. 浙东白垩纪北漳和梁弄花岗岩体及其暗色岩石包体研究. 高校地质学报, 11 (2): 264-275. https://www.cnki.com.cn/Article/CJFDTOTAL-GXDX200502014.htm
陈志广, 张连昌, 万博, 等, 2008. 内蒙古乌奴格吐山斑岩铜钼矿床低Sr-Yb型成矿斑岩地球化学特征及地质意义. 岩石学报, 24 (1): 115-128. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200801010.htm
陈志广, 张连昌, 周新华, 等, 2006. 满洲里新右旗火山岩剖面年代学和地球化学特征. 岩石学报, 22: 2971-2986. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200612013.htm
邓希光, 李献华, 刘义茂, 等, 2005. 骑田岭花岗岩体的地球化学特征及其对成矿的制约. 岩石矿物学杂志, 24 (2): 93-102. https://www.cnki.com.cn/Article/CJFDTOTAL-YSKW200502001.htm
方向阳, 戴平云, 吴世华, 2005. 湖南沅陵唐浒坪矿田成矿条件分析. 华南地质与矿产, (1): 41-46.
付建明, 谢才富, 彭松柏, 等, 2006. 湖南骑田岭花岗岩及其暗色微粒包体的地球化学与壳幔岩浆的混合作用. 地球学报, 27 (6): 557-569. https://www.cnki.com.cn/Article/CJFDTOTAL-DQXB200606005.htm
葛文春, 吴福元, 周长勇, 等, 2007. 兴蒙造山带东段斑岩型Cu, Mo矿床成矿时代及其地球动力学意义. 科学通报, 52 (20): 2407-2417. https://www.cnki.com.cn/Article/CJFDTOTAL-KXTB200720014.htm
顾晟彦, 华仁民, 戚华文, 2007. 广西新路-水岩坝钨锡矿田的成因探讨. 矿床地质, 26 (3): 265-276. https://www.cnki.com.cn/Article/CJFDTOTAL-KCDZ200703002.htm
黄美, 2003. 福建建宁黄埠地区金矿化基本特征. 福建地质, 22 (3): 131-139. https://www.cnki.com.cn/Article/CJFDTOTAL-FJDZ200303003.htm
黄仁生, 邱盛安, 李昭升, 等, 1999. 福建肖坂韧性剪切带型金矿特征及成因探讨. 福建地质, 18 (4): 178-188. https://www.cnki.com.cn/Article/CJFDTOTAL-FJDZ199904001.htm
贾大成, 胡瑞忠, 赵红军, 等, 2003. 湘东北中生代望湘花岗岩体岩石地球化学特征及其构造环境. 地质学报, 77: 98-103. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE200301019.htm
蒋少涌, 赵葵东, 姜耀辉, 等, 2006. 华南与花岗岩有关的一种新类型的锡成矿作用: 矿物化学、元素和同位素地球化学证据. 岩石学报, 22 (10): 2509-2516. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200610010.htm
金成伟, Harris, N. B. W., 许荣华, 等, 1990. 拉萨至格尔木的深成岩. 见: 青藏高原地质演化. 北京: 科学出版社, 141-173.
金维俊, 张旗, 何登发, 等, 2005. 西秦岭埃达克岩的SHRI MP定年及其构造意义. 岩石学报, 21 (3): 959-966. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200503034.htm
康如华, 2001. 湖南掉水洞微细粒浸染型金矿控矿特征. 地质与资源, 10 (4): 210-214. https://www.cnki.com.cn/Article/CJFDTOTAL-GJSD200104003.htm
冷成彪, 张兴春, 陈衍景, 等, 2007. 中国斑岩铜矿与埃达克(质) 岩关系探讨. 地学前缘, 14 (5): 199-210. https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY200705022.htm
李承东, 张旗, 苗来成, 等, 2004. 冀北中生代高Sr低Y和低Sr低Y型花岗岩: 地球化学、成因及其与成矿作用的关系. 岩石学报, 20 (2): 269-284. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200402008.htm
李福顺, 康如华, 陈贻旺, 等, 2002. 湖南高家坳金矿床成矿地质条件及找矿方向. 黄金, 23 (5): 1-3. https://www.cnki.com.cn/Article/CJFDTOTAL-HJZZ200205000.htm
李淼, 张成立, 苑克增, 等, 2004. 南秦岭迷坝岩体的地球化学特征及其地质意义. 西北大学学报(自然科学版), 34 (3): 325-330. https://www.cnki.com.cn/Article/CJFDTOTAL-XBDZ200403022.htm
李鹏春, 许德如, 陈广浩, 等, 2005. 湘东北金井地区花岗岩成因及地球动力学暗示: 岩石学、地球化学和Sr-Nd同位素制约. 岩石学报, 21 (3): 921-934. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201506007.htm
刘红涛, 张旗, 刘建明, 等, 2004. 埃达克岩与斑岩铜矿-浅成热液金矿: 有待深入研究的岩浆成矿关系. 岩石学报, 20 (2): 205-218. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200402002.htm
卢克标, 2004. 福建建瓯奖坑金矿地质地球化学特征及预测评价. 福建地质, 23 (2): 104-109. https://www.cnki.com.cn/Article/CJFDTOTAL-FJDZ200402009.htm
吕贻峰, 1997. 辽南地区(庄河-丹东) 中生代花岗岩类成因特征及其与金矿关系. 辽宁地质, (4): 292-302.
罗铭玖, 黎世美, 卢欣祥, 等, 2000. 河南省主要矿产的成矿作用及矿床系列. 北京: 地质出版社, 1-355.
马丽艳, 路远发, 梅玉萍, 等, 2006. 湖南水口山矿区花岗闪长岩中的锆石SHRI MP U-Pb定年及其地质意义. 岩石学报, 22 (10): 2475-2482. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201501005.htm
马铁球, 王先辉, 柏道远, 2004. 锡田W, Sn花岗岩体的地球化学特征及其形成构造背景. 华南地质与矿产, (1): 11-16.
毛建仁, 许乃政, 胡青, 等, 2004. 福建省上杭—大田地区中生代成岩成矿作用与构造环境演化. 岩石学报, 20 (2): 285-296. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200402009.htm
毛景文, 谢桂青, 张作衡, 等, 2005. 中国北方中生代大规模成矿作用的期次及其地球动力学背景. 岩石学报, 21 (1): 169-188. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200501018.htm
彭渤, 黄瑞华, 1996. 湖南岩金矿床找矿前景的构造成矿研究. 地质地球化学, (1): 56-60.
彭头平, 席先武, 王岳军, 等, 2004. 湘东北早中生代花岗闪长岩地球化学特征及其构造意义. 大地构造与成矿学, 28 (3): 287-296. https://www.cnki.com.cn/Article/CJFDTOTAL-DGYK200403008.htm
钱存超, 路玉林, 刘丽利, 2004. 大别山超高压变质带燕山期花岗岩地球化学特征及成因探讨. 中国地质, 31 (2): 147-154. https://www.cnki.com.cn/Article/CJFDTOTAL-DIZI200402004.htm
秦克章, 李惠民, 李伟实, 等, 1999. 内蒙古乌奴格吐山斑岩铜钼矿床的成岩、成矿时代. 地质论评, 45 (2): 180-185. https://www.cnki.com.cn/Article/CJFDTOTAL-DZLP199902014.htm
芮宗瑶, 侯增谦, 李光明, 等, 2006. 俯冲、碰撞、深断裂和埃达克岩与斑岩铜矿. 地质与勘探, 42 (1): 1-6. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKT200601000.htm
隋振民, 葛文春, 吴福元, 等, 2007. 大兴安岭东北部侏罗纪两类花岗岩的锆石U-Pb年龄、地球化学特征及成因. 岩石学报, 23: 461-480. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200702024.htm
谭俊, 魏俊浩, 李艳军, 等, 2007. 南岭中生代陆壳重熔型花岗岩类成岩成矿的有关问题. 地质论评, 53 (3): 349-362. https://www.cnki.com.cn/Article/CJFDTOTAL-DZLP200703007.htm
王晓勇, 赵春荣, 王振宇, 等, 2004. 大兴安岭北部金矿床类型及地质特征. 黄金地质, 10 (2): 50-54. https://www.cnki.com.cn/Article/CJFDTOTAL-HJDZ200402009.htm
汪雄武, 王晓地, 刘家齐, 等, 2004. 湖南骑田岭花岗岩与锡成矿的关系. 地质科技情报, 23 (2): 1-12. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ200402000.htm
汪雄武, 王晓地, 2001. 花岗岩成矿的地球化学判别标志. 华南地质与矿产, (4): 36-44.
汪洋, 2002. 中国东部燕山期强过铝质花岗岩的地球动力学意义——以冀晋辽地区和广东吴川-四会地区为例. 北京地质, 14 (3): 1-10. https://www.cnki.com.cn/Article/CJFDTOTAL-JBDZ200203000.htm
汪洋, 2009. 北京白查A型花岗岩的地球化学特征及其成因与构造指示意义. 岩石学报, 25 (1): 13-24. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200901003.htm
王岳军, 范蔚茗, 梁新权, 等, 2005. 湖南印支期花岗岩SHRI MP锆石U-Pb年龄及其成因启示. 科学通报, 50: 1259-1266. https://www.cnki.com.cn/Article/CJFDTOTAL-KXTB200512017.htm
王义天, 毛景文, 卢欣祥, 等, 2002. 河南小秦岭金矿区Q875脉中深部矿化蚀变岩的40Ar-39Ar年龄及其意义. 科学通报, 47: 1427-1431. https://www.cnki.com.cn/Article/CJFDTOTAL-KXTB200218015.htm
王治华, 吴兴泉, 王科强, 等, 2006. 西藏申扎西南部甲岗雪山钨钼(铋) 矿区嘎若二长花岗岩体的地球化学特征. 地质通报, 25 (12): 1487-1491. https://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD200612018.htm
魏春生, 郑永飞, 赵子福, 2001. 中国东部A型花岗岩形成时代及物质来源的Nd-Sr-O同位素地球化学制约. 岩石学报, 17 (1): 95-111. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200101009.htm
魏君奇, 战明国, 路远发, 等, 1997. 滇西德钦羊拉矿区花岗岩类地球化学. 华南地质与矿产, (4): 50-56.
武广, 陈衍景, 孙丰月, 等, 2008. 大兴安岭北端晚侏罗世花岗岩类地球化学及其地质和找矿意义. 岩石学报, 24: 899-910. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200804029.htm
伍光英, 潘仲芳, 李金冬, 等, 2005. 湘南大义山花岗岩地质地球化学特征及其与成矿的关系. 中国地质, 32 (3): 434-442. https://www.cnki.com.cn/Article/CJFDTOTAL-DIZI200503012.htm
谢才富, 朱金初, 丁式江, 等, 2006. 海南尖峰岭花岗岩体的形成时代、成因及其与抱伦金矿的关系. 岩石学报, 22 (10): 2493-2508. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200610009.htm
谢新泉, 张衡龙, 2005. 湖南城步县金水铜矿地质特征及成因探讨. 华南地质与矿产, (1): 37-40.
徐启东, 钟增球, 周汉文, 等, 1998. 豫西西秦岭金矿区的一组40Ar/39Ar定年数据. 地质论评, 44: 323-327. https://www.cnki.com.cn/Article/CJFDTOTAL-DZLP199803018.htm
徐夕生, 邓平, O Reilly, S. Y. O., 等, 2003. 华南贵东杂岩体单颗粒锆石激光探针定年及其成岩意义. 科学通报, 48: 1328-1334. https://www.cnki.com.cn/Article/CJFDTOTAL-KXTB200312020.htm
杨进辉, 朱美妃, 刘伟, 等, 2003. 胶东地区郭家岭花岗闪长岩的地球化学特征及成因. 岩石学报, 19: 692-700. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200304009.htm
姚军明, 华仁民, 林锦富, 2005. 湘东南黄沙坪花岗岩LA-ICPMS锆石U-Pb定年及岩石地球化学特征. 岩石学报, 21 (3): 688-696. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200503011.htm
叶会寿, 毛景文, 李永峰, 等, 2006. 东秦岭东沟超大型斑岩钼矿SHRI MP锆石U-Pb和辉钼矿Re-Os年龄及其地质意义. 地质学报, 80 (7): 1078-1088. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE200607013.htm
雍永源, 2007. 锡和钨: 西藏冈底斯带潜在的优势矿种. 沉积与特提斯地质, 27: 1-8. https://www.cnki.com.cn/Article/CJFDTOTAL-TTSD200701000.htm
余阳春, 伍式崇, 梁铁刚, 2006. 锡田地区成矿地质特征及找矿方向. 资源调查与环境, 27 (2): 136-142. https://www.cnki.com.cn/Article/CJFDTOTAL-HSDZ200602008.htm
曾普胜, 李文昌, 王海平, 等, 2006. 云南普朗印支期超大型斑岩铜矿床: 岩石学及年代学特征. 岩石学报, 22 (4): 989-1000. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200604022.htm
詹发余, 古凤宝, 李东生, 等, 2007. 青海东昆仑埃达克岩的构造环境及成矿意义. 地质学报, 81 (10): 1352-1368. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE200710007.htm
张成立, 罗静兰, 李淼, 等, 2002. 东秦岭西坝花岗岩体及其脉岩的地球化学特征. 西北大学学报(自然科学版), 32 (4): 384-388. https://www.cnki.com.cn/Article/CJFDTOTAL-XBDZ200204020.htm
张宏飞, 靳兰兰, 张利, 等, 2005. 西秦岭花岗岩类地球化学和Pb-Sr-Nd同位素组成对基底性质及其构造属性的限制. 中国科学(D辑), 35 (10): 914-926. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK200510001.htm
张宏飞, 肖龙, 张利, 等, 2007. 扬子陆块西北缘碧口块体印支期花岗岩类地球化学和Pb-Sr-Nd同位素组成: 限制岩石成因及其动力学背景. 中国科学(D辑), 37 (4): 460-470. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK200704003.htm
张家菁, 陈郑辉, 王登红, 等, 2008. 福建行洛坑大型钨矿的地质特征、成矿时代及其找矿意义. 大地构造与成矿学, 32 (1): 92-97. https://www.cnki.com.cn/Article/CJFDTOTAL-DGYK200801013.htm
张敏, 陈培荣, 黄国龙, 等, 2006. 南岭龙源坝复式岩体的地球化学特征研究. 铀矿地质, 22 (6): 336-344. https://www.cnki.com.cn/Article/CJFDTOTAL-YKDZ200606002.htm
张旗, 潘国强, 李承东, 等, 2007. 花岗岩结晶分离作用问题——关于花岗岩研究的思考之二. 岩石学报, 23: 1239-1251. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200706001.htm
张旗, 钱青, 王二七, 等, 2001. 燕山中晚期的"中国东部高原": 埃达克岩的启示. 地质科学, 36 (2): 248-255. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKX200102015.htm
张旗, 秦克章, 王元龙, 等, 2004. 加强埃达克岩研究, 开创中国Cu、Au等找矿工作的新局面. 岩石学报, 20: 195-204. https://cpfd.cnki.com.cn/Article/CPFDTOTAL-DZDQ200412002054.htm
张旗, 王焰, 李承东, 等, 2006. 花岗岩的Sr-Yb分类及其地质意义. 岩石学报, 22 (9): 2249-2269. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200609000.htm
张旗, 王元龙, 张福勤, 等, 2002. 埃达克岩与斑岩铜矿. 华南地质与矿产, (3): 85-90.
张旗, 王元龙, 金惟俊, 等, 2008a. 造山前、造山和造山后花岗岩的识别. 地质通报, 27 (1): 1-18. https://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD200801002.htm
张旗, 王焰, 金惟俊, 等, 2008b. 早中生代的华北北部山脉: 花岗岩的证据. 地质通报, 27 (9): 1391-1403. https://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD200809005.htm
张旗, 王元龙, 金惟俊, 等, 2008c. 晚中生代的中国东部高原: 证据、问题和启示. 地质通报, 27 (9): 1404-1330. https://cpfd.cnki.com.cn/Article/CPFDTOTAL-DZDQ200901001345.htm
张旗, 王焰, 熊小林, 等, 2008d. 埃达克岩和花岗岩: 挑战与机遇. 北京: 中国大地出版社.
张田, 张岳桥, 2007. 胶东半岛中生代侵入岩浆活动序列及其构造制约. 高校地质学报, 13 (2): 323-336. https://www.cnki.com.cn/Article/CJFDTOTAL-GXDX200702014.htm
赵广涛, 曹钦臣, 王德滋, 等, 1997. 崂山花岗岩锆石U-Pb年龄测定及其意义. 青岛海洋大学学报(自然科学版), 27 (3): 382-388. https://www.cnki.com.cn/Article/CJFDTOTAL-QDHY703.016.htm
赵建光, 唐卫国, 谢朝晖, 2004. 湖南雪峰金矿田地球化学异常特征及其指示意义. 黄金, 25 (9): 11-14. https://www.cnki.com.cn/Article/CJFDTOTAL-HJZZ200409003.htm
赵书跃, 韩彦东, 朱春燕, 等, 2004. 大兴安岭火山喷发带北段中性、中酸性火山岩地球化学特征及其地质意义. 地质力学学报, 10: 276-287. https://www.cnki.com.cn/Article/CJFDTOTAL-DZLX200403009.htm
赵希林, 2007. 福建省上杭地区中生代花岗岩体的年代学、岩石学、地球化学特征及其地质意义(学位论文). 北京: 中国地质科学院.
赵振华, 王强, 熊小林, 等, 2006. 新疆北部的两类埃达克岩. 岩石学报, 22 (5): 1249-1265. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200605016.htm
周乐尧, 邱郁双, 1997. 浙江中生代陆缘火山岩金矿成矿系统. 浙江地质, 13 (2): 11-21. https://www.cnki.com.cn/Article/CJFDTOTAL-ZJDZ199702002.htm
祝洪臣, 张炯飞, 权恒, 2005. 大兴安岭中生代两期成岩成矿作用的元素、同位素特征及其形成环境. 吉林大学学报(地球科学版), 35: 436-442. https://www.cnki.com.cn/Article/CJFDTOTAL-CCDZ200504004.htm