地球科学进展 ›› 2014, Vol. 29 ›› Issue (12): 1372 -1382. doi: 10.11867/j.issn.1001-8166.2014.12.1372

综述与评述 上一篇    下一篇

中国东部中生代流纹岩—粗面岩组合与热液型铀矿研究新进展
巫建华 1, 解开瑞 2, 吴仁贵 2, 郭国林 1, 刘帅 1   
  1. 1.东华理工大学核资源与环境国家重点实验室培育基地,江西 南昌 330013; 2.东华理工大学地球科学学院,江西 南昌 330013
  • 收稿日期:2014-05-23 修回日期:2014-09-23 出版日期:2014-12-20
  • 基金资助:

    国家自然科学基金项目“沽源—红山子铀成矿带流纹岩—粗面岩组合的成因及其与铀成矿的关系”(编号:41372071); 中国核工业集团公司项目“中国中—新生代铀成矿作用研究”(编号:中核地计[2008]74号)资助

The New Progress in the Study of Mesozoic Rhyolite-Trachyte Assemblage and Hydrothermal-type Uranium Mineralization in Eastern China

Wu Jianhua 1, Xie Kairui 2, Wu Rengui 2, Guo Guolin 1, Liu Shuai 1   

  1. 1.State Key Laboratory Breeding Base of Nuclear Resources and Environment, East China Institute of Technology, Nanchang 330013, China; 2.College of Earth Science, East China Institute of Technology, Nanchang 330013, China
  • Received:2014-05-23 Revised:2014-09-23 Online:2014-12-20 Published:2014-12-20

中国东部中生代火山活动强烈,热液型铀矿分布广泛。空间上,自北而南可划分出大兴安岭、小兴安岭—张广才岭、冀北—辽西、长江中下游、赣杭、武夷山区和东南沿海7个火山岩带和满洲里—额尔古纳、扎兰屯、伊春、沽源—红山子、青龙—兴城、庐枞—栖霞、赣杭和武夷山8个铀成矿带或铀成矿远景带;时间上,从早到晚可划分出早侏罗世—中侏罗世早期、中侏罗世晚期—晚侏罗世早期、早白垩世早期、早白垩世中期、早白垩世晚期和晚白垩世早期6个不同时期的岩石组合,其中早白垩世早期高钾钙碱性流纹岩—碱性粗面岩组合与已知铀矿关系密切,高钾钙碱性流纹岩能为浅成低温成矿系统提供铀,碱性粗面岩可能是深源高温成矿系统富铀碱性成矿流体的开路先锋。

The most intense area of Mesozoic volcanism and main region of hydrothermal-type uranium deposits is located in Eastern China. From the northern to the southern part, it can be divided into seven volcanic belts of Great Xing’an Range, Lesser Xing’an-Zhangguangcai Ranges, Northern Hebei-Western Liaoning, the Lower Yangtze Region, Ganhang areas, Wuyi Mountain areas,the Southeast Coastal areas, five uranium metallogenic belts of Guyuan-Hongshanzi, Qinglong-Xingcheng, Luzong-Qixia, Ganhang, Wuyi Mountain, and Three uranium metallogenic perspective belts of Manzhouli-Erguna, Zhalantun, Yichun. The volcanism of all these volcanic belts can be subdivided into six stages: The Early Jurassic to early Middle Jurassic, late Middle Jurassic to early Late Jurassic, early Early Cretaceous, middle Early Cretaceous, late Early Cretaceous and early Late Cretaceous. High-K calc-alkaline rhyolite-alkali trachyte rock assemblage of the early Early Cretaceous has a close connection with the explored uranium deposits. High-K calc-alkaline rhyolites have high content of uranium, and can provide the epithermal ore forming system with uranium; Alkali trachyte associated with mantle-derived magmatism can provide alkaline ore-forming fluid of rich uranium for deep temperature mineralizing system or act as pioneers of alkaline ore-forming fluid of rich uranium.

中图分类号: 

[1] Zhang Jindai,Li Ziying,Cai Yuqi,et al.The main advance and achievements in the potential evalution of uranlum resource in China[J].Uranium Geology, 2012, 28(6):321-326. [张金带,李子颖,蔡煜琦,等.全国铀矿资源潜力评价工作进展与主要成果[J].铀矿地质, 2012,28(6):321-326.]
[2] Ji Chunyu,Wu Jianhua. The SHRIMP zircon U-Pb dating of felsic volcanic rocks and its geological significance from Yutian Group in southern Jiangxi[J]. Journal of East China Institute of Technology, 2010, 33(2):131-138. [冀春雨,巫建华.江西南部余田群长英质火山岩SHRIMP锆石U-Pb年龄及其地质意义[J].东华理工大学学报:自然科学版, 2010,33(2): 131-138.]
[3] Xiang Yuanxin, Wu Jianhua. SHRIMP zircon U-Pb age of Yutian Group basalts in Longnan area of southern Jiangxi Province and its geological significance[J]. Geological Bulletin of China, 2012,31(5):716-725. [项媛馨,巫建华.赣南龙南地区余田群玄武岩SHIRMP锆石U-Pb年龄及其地质意义[J].地质通报, 2012,31(5): 716-725.]
[4] Zhu Yudi, Ye Xifang, Zhang Dehui,et al. A comparative study of granites in Tongcun porphyry molybdenum-copper deposit in west of Zhejiang Province and Dexing porphyriry copper Deposit[J].Advances in Earth Science, 2012,27(10):1 043-1 053. [朱玉娣,叶锡芳,张德会,等.浙西桐村斑岩型钼(铜)矿床与德兴斑岩铜矿岩浆岩对比研究[J]. 地球科学进展,2012, 27(10):1 043-1 053.]
[5] Yang W, Li S G. Geochronology and geochemistry of the Mesozoic volcanic rocks in Western Liaoning: Implications for lithospheric thinning of the North China craton[J].Lithos, 2008, 102(1/2):88-117.
[6] Zhang J H,Ge W C, Wu F Y, et al. Large-scale Early Cretaceous volcanic events in the northern Great Xing’an Range, Northeastern China[J]. Lithos, 2008, 102:138-157.
[7] Zhang J H, Gao S, Ge W C, et al. Geochronology of the Mesozoic volcanic rocks in the Great Xing, an Range, northeastern China: Implications for subduction-induced delamination[J].Chemical Geology, 2010, 276: 144-165.
[8] Ma Qiang,Zheng Jianping.In-situ U-Pb dating and Hf isotopic analyses of zircons in the volcanic rock of the Lanqi Formation in the Beipiao area, western Liaoning Province[J]. Acta Petrologica Sinica, 2009, 25(12):3287-3297. [马强,郑建平.辽西北票蓝旗组火山岩锆石U-Pb年龄和Hf同位素组成[J].岩石学报, 2009,25(12):3 287-3 297.]
[9] Li Ke, Zhang Zhicheng, Li Jianfeng, et al. Zircon SHRIMP U-Pb age and geochemical characteristics of the Mesozoic volcanic rocks in Xi Ujimqin Banner, Inner Mongolia[J]. Geological Bulletin of China, 2012,31(5): 671-685. [李可,张志诚,李建锋,等. 内蒙古西乌珠穆沁旗地区中生代中酸性火山岩SHRIMP锆石U-Pb年龄和地球化学特征[J].地质通报, 2012,31(5):671-685.]
[10] Wu Jianhua, Wu Jun, Zhu Hongtao, et al. Lithostratigraphical correlation of the volcanic rock series in Hongshanzi Basin in Great Hingan Range[J].Geological Journal of China Universities, 2013,19(3):472-483. [巫建华,武珺,祝洪涛,等.大兴安岭红山子盆地火山岩系岩石地层对比[J].高校地质学报,2013.19(3):472-483.]
[11] Ying J F, Zhou X H, Zhang L C, et al. Geochronological and geochemical investigation of the late Mesozoic volcanic rocks from the Northern Great Xing’an Range and their tectonic implications[J]. International Journal of Earth Sciences, 2010, 99(2):357-378.
[12] Li Pingping, Ge Wenchun, Zhang Yanlong. Division of volcanic strata in the northwestern part of Hailar Basin: Evidence fromzircon U-Pb dating[J]. Acta Petrologica Sinica, 2010,26(8):2 482-2 494. [李萍萍,葛文春,张彦龙.海拉尔盆地西北部火山岩地层划分的锆石U-Pb年代学证据[J].岩石学报,2010, 26(8):2482-2494.]
[13] Meng En,Xu Wenliang,Yang Debin, et al. Zircon U-Pb chronology, geochemistry of Mesozoicvolcanic rocks from the Lingquan Basin in Manzhouli area,and its tectonic implications[J]. Acta Petrologica Sinica, 2011, 27(4):1 209-1 226. [孟恩,许文良,杨德彬,等.满洲里地区灵泉盆地中生代火山岩的锆石U-Pb年代学、地球化学及其地质意义[J].岩石学报,2011,27(4):1209-1226.]
[14] Zhou Taofa, Fan Yu, Yuan Feng, et al. Geochronology and significance of volcanic rocks in the Ning-Wu Basin of China[J]. Science in China(Series D), 2011, 54(2):185-196. [周涛发,范裕,袁峰,等.宁芜(南京—芜湖)盆地火山岩的年代学及其意义[J].中国科学:D辑,2011,41(7): 960-971.]
[15] Zhou Taofa, Fan Yu, Yuan Feng, et al. Geochronology and significance of volcanic rocks in the Lu-Zong Basin of China[J]. Science in China (Series D), 2008,38(11): 1342-1353. [周涛发,范裕,袁峰,等.安徽庐枞(庐江—枞阳)盆地火山岩的年代学及其意义[J].中国科学:D辑, 2008,38(11): 1342-1353.]
[16] Yan Jun, Liu Haiquan, Song Chuanzhong, et al. Zircon U-Pb geochronology of the volcanic rocks from Fanchang-Ningwu volcanic basins in the Lower Yangtze region and its geological implications[J]. Chinese Science Bulletin, 2009, 54(12):1716-1724. [闫峻,刘海泉,宋传中,等.长江中下游繁昌—宁芜火山盆地火山岩锆石U-Pb年代学及其地质意义[J].科学通报, 2009,54(12):1716-1724.]
[17] Hou Kejun, Yuan Shunda. Zircon U-Pb age and Hf isotopic composition of the volcanic and sub-volcanic rocks in the Ningwu Basin and their geological implications[J].Acta Petrologica Sinica, 26(3): 888-902 [侯可军,袁顺达.宁芜盆地火山—次火山岩的锆石U-Pb年龄、Hf 同位素组成及其地质意义[J].岩石学报,2010, 26(3):888-902.]
[18] Xie Chenglong, Zhu Guang, Niu Manlan, et al. LA-ICP MS Zircon U-Pb ages of the Mesozoic volcanic rocks from Chuzhou area and their tectonic significances [J]. Geological Review, 2007, 53(5): 642-655. [谢成龙,朱光,牛漫兰,等.滁州中生代火山岩LA- ICP-MS锆石U-Pb 年龄及其构造地质学意义[J].地质论评, 2007, 53(5): 642-655.]
[19] Yuan Feng, Zhou Taofa, Fan Yu, et al. LA-ICPMS U-Pb ages of zircons from Mesozoic volcanic rocks and their significance in Fanchang Basin, Anhui Province, China[J].Acta Petrologica Sinica, 2010, 26(9): 2 805-2 817. [袁峰,周涛发,范裕,等.安徽繁昌盆地中生代火山岩锆石LA-ICP MS U-Pb 年龄及其意义[J].岩石学报, 2010,26(9): 2 805-2 817.]
[20] Ma Fang, Xue Huaimin. SHRIMP zircon U-Pb age of late Mesozoic volcanic rocks from the Chuzhou Basin, eastern Anhui Province, and its geological significance[J]. Acta Petrologica Etmineralogica, 2011,30(5):924-934. [马方,薛怀民.皖东滁州盆地晚中生代火山岩的SHRIMP锆石U-Pb年龄及其地质意义[J]. 岩石矿物学杂志, 2011,30(5): 924-934.]
[21] Yang Shuiyuan, Jiang Shaoyong, Jiang Yaohui, et al. Zircon U-Pb geochronology, Hf isotopic composition and geological implications of the rhyodacite and rhyodacitic porphyry in the Xiangshan uranium ore field, Jiangxi Province, China[J]. Science in China (Series D), 2010, 40(8):953-969. [杨水源,蒋少涌,姜耀辉,等.江西相山流纹英安岩和流纹英安斑岩锆石U-Pb年代学和Hf同位素组成及其地质意义[J].中国科学: D辑, 2010,40(8):953-969.]
[22] Gou Jun,Sun Deyou, Zhao Zhonghua, et al. Zircon LA-ICPMS U-Pb dating and petrogenesis of rhyolites in Baiyingaolao Formation from the southern Manzhouli, Inner-Mongolia[J]. Acta Petrologica Sinica, 2010, 26(1):333-344. [苟军,孙德有,赵忠华,等.满洲里南部白音高老组流纹岩锆石U-Pb定年及岩石成因[J].岩石学报, 2010,26(1): 333-344.]
[23] Wu Jianhua, Liu Feiyu, Liu Shuai. SHRIMP U-Pb zircon age of Late Mesozoic trachyte in Xiajiang-Guangfeng and Sannan(Quannan, Dingnan and Longnan)-Xunwu volcanic belts[J]. Geological Review, 2011,57(1):125-132. [巫建华,刘飞宇,刘帅.峡江—广丰和三南—寻乌火山岩带晚中生代粗面岩SHRIMP锆石U-Pb年龄[J].地质论评, 2011,57(1): 125-132.]
[24] Wu Jianhua, Xiang Yuanxin, Liu Shuai. Wuyi Group of douthern Jiangxi and its geological age[J]. Journal of Stratigraphy, 2011,35(2):200-208. [巫建华,项媛馨,刘帅.江西南部武夷群及其地质时代[J].地层学杂志,2011,35(2):200-208.]
[25] Su Huimin, He Xirong. Timing of the formation of the Tianhuashan Basin in northern Wuyi as constrained by geochronology of volcanic rocks[J]. Acta Mineralogica Sinica, 2011,(Suppl.):635-636. [苏慧敏,何细荣.北武夷天华山盆地形成时限的约束:来自火山岩的年代学证据[J].矿物学报,2011,(增刊):635-636.]
[26] Zhang Hong, Liu Xiaoming, Yuan Honglin, et al. U-Pb isotopic age of the lower Yixian Formation in Lingyuan of western Liaoning and its significance[J]. Geological Review, 2006,24(2): 63-71. [张宏,柳小明, 袁洪林,等.辽西凌源地区义县组下部层位的U-Pb测年及意义[J].地质论评, 2006,24(2): 63-71.]
[27] Zhang Hong, Liu Xiaoming, Chen Wen, et al. The age of the top of the Yixian Formation in the Beipiao-Yixian area, western Liaoning, and its importance[J].Geology in China,2005, 32(4):596-603. [张宏,柳小明,陈文,等.辽西北票—义县地区义县组顶部层位的年龄及其意义[J].中国地质,2005, 32(4):596-603.]
[28] Wu Huaying, Zhang Lianchang, Zhou Xinhua, et al. Geochronology and geochemical characteristics of Late Mesozoic Da-Hinggan Mountains, and its genesis[J]. Acta Petrologica Sinica, 2008,24(6):1 339-1 352. [吴华英,张连昌,周新华,等.大兴安岭中段晚中生代安山岩年代学和地球化学特征及成因分析[J].岩石学报,2008,24(6): 1339-1352.]
[29] Xing Guangfu, Lu Qingdi, Chen Rong, et al. Study on the ending time of Late Mesozoic tectonic regime transition in South China—Comparing to the Yanshan area in North China[J].Acta Geologica Sinica, 2008, 82(4):451-463. [邢光福,卢清地,陈荣,等.华南晚中生代构造体制转折结束时限研究——兼与华北燕山地区对比[J].地质学报, 2008,82(4):451-463.]
[30] Meng Fanxue, Gao Shan, Liu Xiaoming. U-Pb zircon geochronology and geochemistry of volcanic rocks of the Yixian Formation in the Lingyuan area, western Liaoning, China[J]. Geological Bulletin of China, 2008,27(3):364-373. [孟凡雪,高山,柳小明.辽西凌源地区义县组火山岩锆石U-Pb年代学和地球化学特征[J].地质通报,2008,27(3):364-373.]
[31] Cui Yurong, Xie Zhi, Chen Jiangfeng, et al. SHRIMP U-Pb dating of zircons from the Late Mesozoic basalts in Eastern Zhejiang Province and its geological significance[J]. Geological Journal of China Universities, 2010,16(2):198-212. [崔玉荣,谢智,陈江峰,等.浙东晚中生代玄武岩的锆石SHRIMP U-Pb年代学及其地质意义[J].高校地质学报,2010,16(2): 198-212.]
[32] Shu Liangshu, Deng Ping, Wang Bin, et al. Lithology, kinematics and geochronology related to Late Mesozoic basin-mountain evolution in the Nanxiong-Zhuguang area, South China[J]. Science in China (Series D), 2004,47(8):673-688. [舒良树,邓平,王彬,等.南雄—诸广地区晚中生代盆山演化的岩石化学、运动学与年代学制约[J].中国科学:D辑, 2004,34(1):1-13.]
[33] Li Ruiling, Li Zhenzhen. SHRIMP zircon U-Pb age of Late Mesozoic basaltic asaltic magmatism in the Yujiang region, southeastern China and its implication[J]. Journal of Mineralogy and Petrology, 2010,30(2): 45-49. [李瑞玲,李真真.中国东南部余江基性岩体的SHRIMP锆石U-Pb年龄及其地质意义[J].矿物岩石, 2010,30(2):45-49.]
[34] Wu Jianhua, Xu Xunsheng, Liu Shuai. SHRIMP zircon U-Pb dating of the early Late Cretaceous felsic volcanic rock in southern Jiangxi-northern Guangdong area and its geological significance[J]. Geological Bulletin of China, 2012,31(8):1 296-1 305. [巫建华,徐勋胜,刘帅.赣南—粤北地区晚白垩世早期长英质火山岩SHIRMP锆石U-Pb年龄及其地质意义[J]. 地质通报, 2012,31(8): 1 296-1 305.]
[35] Wu Jianhua, Xiang Yuanxin, Zhong Zhifei. SHRIMP Zircon U-Pb dating and Sr-Nd-Pb-O isotope characteristics of shoshonite from Guangfeng and Yushan Basins in Jiangxi Province[J]. Acta Petrologica et Mineralogica,2014,33(4):645-656. [巫建华,项媛馨,钟志菲.江西广丰、玉山盆地橄榄玄粗岩的SHRIMP锆石U-Pb定年和Sr-Nd-Pb-O元素同位素特征[J].岩石矿物学杂志, 2014,33(4):645-656.]
[36] Kurt M A, Alpaslan M,Göncüoglu M C, et al. Geochemistry of late stage medium to High-K Calc-Alkaline and shoshonitic dykes in the ulukisla sasin (Central Anatolia,Turkey): Petrogenesis and tectonic setting[J]. Geochemistry Internationai, 2008, 46(11):1145-1163.
[37] Li Wuping, Li Xianhua. Petrogenesis and its implication for the middle-late Jurassic intermediate-acidic volcanic rocks in the middle section of Yanshan orogen[J]. Acta Petrologica Sinica, 2004,20(3):501-510. [李伍平,李献华.燕山造山带中段中晚侏罗世中酸性火山岩的成因及其意义[J].岩石学报, 2004,20(3):501-510.]
[38]Feng Guangying, Liu Shen, Zhong Hong, et al. Zricon U-Pb age, geochemical characteristics and petrogenesis of the Yixian Formation volcanic rocks in Jianchang,Western Liaoning Province[J].Acta Mineralogica Sinica, 2011, 31(3):380-390. [冯光英,刘燊,钟宏,等.辽西建昌碱性粗面岩的年代学及岩石成因研究[J].矿物学报, 2011,31(3):380-390.]
[39] Deng Jinfu, Liu Cui, Feng Yanfang, et al. Petrology of volcanic rocks and its relationship to Fe-Cu mineralization of Luzong and Chouzhou Basin, Anhui Province[J].Acta Geologica Sinica, 2011, 85(5): 626-635. [邓晋福,刘翠,冯艳芳,等. 安徽省庐枞与滁州盆地火山岩岩石学特征与Fe-Cu成矿的关系[J].地质学报, 2011,85(5):626-635.]
[40] He Zhenyu, Xu Xisheng, Chen Rong, et al. Genesis of Middle Jurassic syenite-gabbro in southern Jiangxi Provence and their geological significance[J]. Acta Petrologica Sinica,2007,23(6):1457-1469. [贺振宇,徐夕生,陈荣,等.赣南中侏罗世正长岩—辉长岩的起源及其地质意义[J].岩石学报,2007,23(6): 1457-1469]
[41] Li Xiaoyong, Guo Feng, Fan Weiming, et al. Early Cretaceous trachytes of Donglingtai Formation from the Xishan area in the northern North China Block: Constraints on melting of lower mafic crust[J]. Geotectonica et Metallogenia, 2004, 28(2): 155-164. [李晓勇,郭锋,范蔚茗,等.北京西山东岭台组粗面质火山岩地球化学: 下地壳熔融成因[J].大地构造与成矿学, 2004,28(2): 155-164.]
[42] Sun Deyou, Gou Jun, Ren Yunsheng, et al. Zircon U-Pb dating and study on geochemistry of volcanic rocks in Manitu Formation from southern Manchuria,Inner Mongolia[J]. Acta Petrologica Sinica, 2011,27(10): 3083-3094. [孙德有, 苟军, 任云生,等.满洲里南部玛尼吐组火山岩锆石 U-Pb 年龄与地球化学研[J].岩石学报, 2011,27(10):3083-3094.]
[43] Xiang Yuanxin, Wu Jianhua. Origin of the Early Cretaceous trachyte in Northern Guangdong Province constraints of Sr-Nd-Pb isotopes[J]. Geological Journal of China Universities, 2011,17(3): 436-446. [项媛馨,巫建华.广东北部早白垩世粗面岩的成因:Sr-Nd-Pb同位素制约[J].高校地质学报,2011,17(3): 436-446.]
[44] Deng Jinfu, Luo Zhaohua, Su Shangguo, et al. The Petrogenesis, Structural Environment and Minerogenesis[M]. Beijing: Geological Publishing House, 2004. [邓晋福,罗照华,苏尚国,等.岩石成因、构造环境与成矿作用[M].北京:地质出版社,2004.]
[45] Li Hongying, Zhang Ronghua, Hu Shumin. Geochemical characteristics of syenite and its genesis in the Luzong Basin[J]. Journal of Jilin University(Earth Science Edition),2009, 39(5):839-848. [李洪英,张荣华,胡书敏.庐枞盆地正长岩类地球化学特征及成因探讨[J].吉林大学学报:地球科学版,2009, 39(5):839-848.]
[46] Li Wuping, Lu Fengxiang, Sun Shanping, et al. Discussion on the origin of volcanic rocks of Donglingtai Formation in Beijing Xishan Mountain and its geological setting[J]. Acta Petrologica Sinica, 2000, 16(3):345-352. [李伍平,路凤香,孙善平,等. 北京西山东岭台组(J 3 ) 火山岩的成因及其构造环境探讨[J].岩石学报, 2000,16(3):345-352.]
[47] Zhang Bangtong, Chen Peirong, Ling Hongfei, et al. Geochemistry and petrogenesis of the middle Jurassic rhyolite, southern Jiangxi: Trace element and Pb-Nd-Sr isotope geochemical constrains on the upper crustal origin[J]. Acta Petrologica Sinica,2004, 20(3):511-520. [章邦桐,陈培荣,凌洪飞,等.赣南中侏罗世流纹岩地球化学及成因研究:上地壳成因的的微量元素和Pb-Nd-Sr同位素地球化学制约[J].岩石学报,2004, 20(3):511-520.]
[48] Wang Jianguo, He Zhonghua, Xu Wenliang. Petrogenesis of riebeckite rhyolites in the southern Da Hinggan Mts. Geohronological and geochemical evidence[J]. Acta Petrologica Sinica, 2013,29(3):853-863. [王建国,和钟铧,许文良.大兴安岭南部钠闪石流纹岩的岩石成因: 年代学和地球化学证据[J].岩石学报,2013,29(3): 853-863.]
[49] Shinjo R, Kato Y. Geochemical constraints on the origin of bimodal magmatism at the Okinawa Trough, an incipient back-arc basin[J].Lithos, 2000,54:117-137.
[50] Gao Xiaofeng, Guo Feng, Li Chaowen, et al. The genesis of two types of Late Mesozoic intermediate-felsic volcanic rocks in Lishui Basin, Lower Yangtze valley[J]. Acta Petrologica Etmineralogica, 2007,26(1):1-12. [高晓峰,郭峰,李超文,等.溧水盆地两类晚中生代中酸性火山岩的岩石成因[J].岩石矿物学杂志,2007,26(1):1-12.]
[51] Li Xianhua, Zhou Hanwen, Li Zhengxiang, et al. Petrogenesis of Neoproterozoic bimodal volcanics in western Sichuan and its tectonic implications:Geochemical and Sm-Nd isotopic constraints[J].Chinese Journal of Geology, 2002, 37(3): 264-276. [李献华,周汉文,李正祥,等.川西新元古代双峰式火山岩成因的微量元素和Sm-Nd同位素制约及其大地构造意义[J].地质科学,2002,37(3): 264-276.]
[52] Briand B,Bouchardon J,Capiez P,et al. Felsic(A-type)-basic(plume-induced) Early Palaeozoic bimodal magmatism in the Maures massif[J].Geological Magazine, 2002, 139(3):291-311.
[53] Wang Dezi, Zhou Xinmin. The Genesis of Late Mesozoic Volcanic Intrusive Complex of Southeast China and Crustal Evolution[M]. Beijing: Science Press, 2002:217-229. [王德滋,周新民.中国东南部晚中生代花岗质火山—侵入杂岩成因与地壳演化[M].北京:科学出版社, 2002:217-229.]
[54] Riley T R,Leat P T,Pankhurst R J,et al. Origins of large volume Rhyolitic volcanism in the Antarctic peninsula and patag-onia by crustal melting[J]. Journal of Petrology,2001,42(6):1043-1065.
[55] Zhang J H, Gao S, Ge W C, et al. Geochronology of the Mesozoic volcanic rocks in the Great Xingan Range, northeastern China: Implications for subduction-induced delamination[J]. Chemical Geology, 2010,276: 144-165.
[56] Wang Rui, Chen Bin, Liu Xiaoming. Geochemical characteristics and origin of the Tiaojishan and Donglingtai Formations from western hills, Beijing[J]. Geological Journal of China Universities, 2007,13(3): 603-612. [王蕊,陈斌,柳小明.北京西山地区髫髻山组和东岭台组火山岩的地球化学特征与岩浆起源[J].高校地质学报, 2007,13(3): 603-612.]
[57] Wang Yang, Ji Guangyi, Sun Shanping, et al. Origin of the volcanic rocks in the Donglingtai Formation from Yanhecheng area, Western Hills of Beijing and its geological implications[J]. Geological Review, 2009, 55(2): 191-214. [汪洋,姬广义,孙善平,等.北京西山沿河城东岭台组火山岩成因及其地质意义[J].地质论评, 2009, 55(2): 191-214.]
[58] Wang Yang, Cheng Suhua. Element geochemistry and petrogenesis of the volcanic rocks of Zhangjiakou formation in the Zhangjiakou area, north China[J].Journal of Mineralogy and Petrology, 2010,30(1):75-82. [汪洋,程素华.张家口地区张家口组火山岩元素地球化学特征及成因[J].矿物岩石, 2010,30(1):75-82.]
[59] Mao Jingwen, Hu Ruizhong, Chen Yuchuan, et al. Studies on the Large-scale Mineralization and Ore district[M]. Beijing:Geological Publishing House, 2006. [毛景文,胡瑞忠,陈毓川,等.大规模成矿作用与大型矿集区[M].北京:地质出版社,2006.]
[60] Huang Shijie. Preliminary discussion on deep-sourced uranium metallogenesis and deep prospecting[J]. Uranium Geology, 2006,22(2): 70-75. [黄世杰.略谈深源铀成矿与深部找矿问题[J].铀矿地质, 2006,22(2):70-75.]
[61]Hu Ruizhong, Li Chaoyang, Ni Shijun, et al. Research on ∑CO 2 source in ore-forming hydrothermal solution of granite-type uranium deposit,South China[J]. Science in China (Series B),1993,36(10):1 252-1 262. [胡瑞忠,李朝阳,倪师军,等.华南花岗岩型铀矿床成矿热液中∑CO 2 来源研究[J].中国科学:B辑, 1993,23(2): 189-196.]
[62] Hu Ruizhong. A commentary on genesis of granite-type uranium deposits: As exemplified by south China[J].Advances in Earth Science, 1994,9(2):41-46. [胡瑞忠.花岗岩型铀矿床成因讨论——以华南为例[J].地球科学进展, 1994,9(2):41-46.]
[63] Li Ziying, Li Xiuzhen, Lin Jinrong. On the Meso-Cenozoic mantle plume tectonics, its relationship to uranium metallogenesis and prospecting directions in south China[J].Uranium Geology, 1999,15(1): 9-17. [李子颖,李秀珍,林锦荣.试论华南中新生代地幔柱构造、铀成矿作用及找矿方向[J].铀矿地质, 1999,15(1): 9-17.]
[64] Fan Honghai, Ling Hongfei, Wang Dezi, et al. Study on metallogenetic mechanism of Xiangshan uranium ore-field[J]. Uranium Geology,2003,19(4):208-213. [范洪海,凌洪飞,王德滋,等.相山铀矿田成矿机理研究[J].铀矿地质, 2003,19(4):208-213.]
[65] Jiang Yaohui, Jiang Shaoyong, Ling Hongfei. Mantle-derived fluids and uranium mineralization[J]. Earth Science Frontiers, 2004,11(2): 491-498. [姜耀辉,蒋少涌,凌洪飞.地幔流体与铀成矿作用[J].地学前缘, 2004,11(2):491-498.]
[66] Wu Jianhua, Liu Shuai, Yu Dagan, et al. Mantle geofluid and uranium ore-formation model[J].Uranium Geology, 2005,21(4):196-203. [巫建华, 刘帅, 余达淦,等.地幔流体与铀成矿模式[J].铀矿地质,2005, 21(4):196-203.]
[67] Chen Youliang,Wei Jia,Ye Yongqin, et al. Significance and geochemical characteristics of ree and carbon-oxygen isotopes of calcites in the zoie uranium orefield in Sichuan Province,China[J].Advances in Earth Science, 2012,27(10):1 061-1 067. [陈友良,魏佳,叶永钦,等.若尔盖铀矿田方解石稀土元素与碳氧同位素地球化学特征及其意义[J].地球科学进展,2012,27(10):1 061-1 067.]
[68] Wu Jianhua, Liu Xiaodong, Zhu Minqiang, et al. Discussion on several problems of deep source of high temperature metallogenic system in Nanling uranium metallogenic belt[M]∥Zhang Jindai,Li Ziying,eds. Uranium Prospecting and Geological Science, Technology Progress and Situation.Beijing:Atomic Energy Press, 2010: 281-376. [巫建华,刘晓东,祝民强,等.南岭铀成矿带深源高温成矿系统的几个问题讨论[M]∥张金带,李子颖.铀矿勘查和地质科技进展与态势.北京:原子能出版社,2010:281-376.]
[69] Du Letian, Wang Wenguang. New exploration target for granite-type uranium deposits in South China—A case study on uranium minerallization of sericitic alteration[J]. Uranium Geology, 2009, 25(2):85-90. [杜乐天,王文广.华南花岗岩型铀矿找矿新目标:绢英岩化铀矿类型[J].铀矿地质, 2009,25(2):85-90.]
[70] Wu Jianhua, Liu Xiaodong, Zhu Minqiang, et al. The Mesozoic volcano activities and uranium mineralization in Eastern China[J]. Acta Mineralogica Sinica, 2011,(Suppl.):303-305. [巫建华,刘晓东,祝民强,等.中国东部中生代火山活动与铀矿成矿作用[J].矿物学报, 2011,(增刊):303-305.]
[71] Ling Hongfei. Origin of hydrothermal fluids of granite-type uranium deposits: Constraints from redox conditions[J]. Geological Review, 2011,57(2):193-206. [凌洪飞.论花岗岩型铀矿床热液来源——来自氧逸度条件的制约[J].地质论评,2011,57(2):193-206.]
[72] Shock E L,Sassani D C, Betz H. Uranium in geologic fluids: Estimates of standard partial molal properties oxidation potentials,and hydrolysis constants at high temperatures and pressures[J]. Geochimica et Cosmochimica Acta, 1997, 61:4 245-4 266.
[73] Liu Congqiang, Li Heping, Huang Zhilong, et al. A review of studies on oxygen fugacity of the earth mantle[J].Earth Science Frontiers, 2001,8(3):73-82. [刘丛强,李和平,黄智龙,等,地幔氧逸度的研究进展[J].地学前缘,2001,8(3):73-82.]
[74] [74]Woodland A B, Koch M. Variationion in oxygen fugacity with depth in the upper mantle beneath the kaapvaal craton,Southern Africa[J]. Earth and Planetary Science Letters, 2003, 214: 295-310.
[75] Dauphas N,Craddock P R,Asimov P D, et al. Iron isotopes may reveal the redox conditions of mantle melting from archean to present[J]. Earth and Planetary Science Letters, 2009,288:255-267.
[76] Farges F,Ponader C W,Calas G, et al. Structural environments of incompatible elments in silicate glass-melt systems:Ⅱ.U Ⅳ ,U Ⅴ ,and U Ⅵ [J]. Geochimica et Cosmochimica Acta, 1992,56:4 205-4 220.
[77] Zhang Yuyan, Li Ziying, Huang Zhizhang, et al. A study on existing forms and migration process of uranium at Shazhou deposit, Jiangxi Province, China: Evidences from induced fission tracks[J]. Geological Journal of China Universities, 2012,18(4):639-646. [张玉燕,李子颖, 黄志章,等.江西相山沙洲矿床铀的存在形式和迁移特征探讨:来自诱发裂变径迹的证据[J].高校地质学报, 2012,18(4):639-646.]

[1] 包汉勇,郭战峰,张罗磊,黄亚平. 太平洋板块形成以来的中国东部构造动力学背景[J]. 地球科学进展, 2013, 28(3): 337-346.
[2] 周广胜,何奇瑾. 生态系统响应全球变化的陆地样带研究[J]. 地球科学进展, 2012, 27(5): 563-572.
[3] 吴德星,兰健. 中国东部陆架边缘海海洋物理环境演变及其环境效应[J]. 地球科学进展, 2006, 21(7): 667-672.
[4] 杨巍然,隋志龙,MatsVD. 俄罗斯贝加尔湖区伸展构造及与中国东部伸展构造对比[J]. 地球科学进展, 2003, 18(1): 45-049.
[5] 沈明洁,谢志仁,朱诚. 中国东部全新世以来海面波动特征探讨[J]. 地球科学进展, 2002, 17(6): 886-894.
[6] 赖彦斌,徐霞,王静爱,王理,于园园,杨春燕. NSTEC不同自然带土地利用/覆盖格局分析[J]. 地球科学进展, 2002, 17(2): 215-220.
[7] 郑度,卢金发. 重视和加强中国东部地区土地退化整治研究[J]. 地球科学进展, 1994, 9(5): 1-5.
阅读次数
全文


摘要