| [1] | 顾连兴,何金祥,胡文宣等.1997.陆壳成熟度对于华南块状硫化物矿床的成分效应.地质学报,71(2)：161～169.
|
| [2] | 隗合明.1990.秦岭凤太铅－锌矿田的海底喷气成矿类型及其空间分布规律.地质论评,36(5)：394～403.
|
| [3] | 缪远兴,冉崇英.1992.内蒙古东升庙铅锌硫矿床海底喷流沉积成矿作用地质地球化学特征.地球化学,21(2)：375～382.
|
| [4] | 李建中,何典仁,吴健民.1992.秦岭型铅－锌矿床.地质学报,66(3)：257～268.
|
| [5] | 李双应,颜怀学,金福全.1993.皖南上震旦统蓝田组缺氧环境的地球化学特征.安徽地质,3(3)：16～21.
|
| [6] | 李双应.1998.皖南上震旦统蓝田组热水沉积物的发现及其意义.安徽地质,8(4)：7～10.
|
| [7] | 涂光炽等.1988.中国层控矿床地球化学(第三卷).北京；地质出版社.152～168.
|
| [8] | 王自强,张玲华,周洪瑞等.1990.扬子地台东南部和北部陆缘区中、晚元古代构造发展特征.见:王鸿祯,杨森楠,刘本培等著.中国及邻区构造古地理和生物古地理.武汉：中国地质大学出版社.246～264.
|
| [9] | 邢凤鸣,徐祥,陈江峰等.1992.江南古陆东南缘晚元古代大陆增生史.地质学报,66(1)：59～72.
|
| [10] | Krebs w.1981.Meggen矿床地质.见：乌尔夫K H主编：层控矿床和层状矿床(第九卷)(中译本).1986.北京：地质出版社.323～352.
|
| [11] | Large D E .1981.沉积岩中的海底喷出铅锌矿床--地质特征和成因评述.见：乌尔夫KH主编：层控矿床和层状矿床(第九卷)(中译本).1986.北京：地质出版社.299～322.
|
| [12] | Meylan M A,Glasby G P,Knedler K E et al.1981.含金属深海沉积物.见：乌尔夫KH主编：层控矿床和层状矿床(第九卷)(中译本).1986.北京：地质出版社.48～114.References
|
| [13] | Bi Zhiguo, Wang Xiafeng, Zhu Hong, Wang Ziqiang, Ding Fang.1988. The Sinian ofSouthern Anhui. In: Professional papers ofstratigraphy and paleontology, No. 19. Beijing:Geological Publishing House. 27～54 (in Chinese).
|
| [14] | Bostrom K. 1973. The origin and fate of ferromanganoan active ridgessediments.Stockholm Contrib. Geology, 27.. 149～243.
|
| [15] | Chen Duofu, Chen Xianpei. 1992. Sedimentary features and origin ofDevonian chertsin Debao, Guangxi, China. Geochimica, 21(2):190～197. (in Chinese with English abstract)
|
| [16] | Chen Duofu, Chen Guangqian, Pan Jingming, Ma Shaogang, DongWeiquan, Gao Jiyuan,Chen Xianpei. 1998. Characterictics ofthe hydrothermal sedimentation of the dajianpingsuperlarge pytitedeposit in Yunfu, Guangdong. Geochimica, 27(1):12～19. (inChinese withEnglish abstract)
|
| [17] | Cronan D S, Moorby S A, Glasby G P, et al. 1984. Hydrothermaland volcaniclasticsedimentaion on the Tonga-Kermadec Ridge andin its adjacent marginal basins. in: KokelaarB P and Howells MF. eds. Marginal Basin Geology. Oxford.. Blackwell ScientificPublication,137～150.
|
| [18] | Fleet A J. 1983. Hydrothermal and hydrogenous ferro-mangan deposits.. Do they forma continuum? in: Rona P A, et al. eds. Therare earth element evidence in hydrothermalprocesses at seafloorspreading center. New York: Plenum Press, 535～555.
|
| [19] | Fouquet Y, Stackelberg U V, Charlou J L, Donval J P, Foucher J P,Erzinger J,Herzig P, Mühe R, Wiedicke M, Soakai S,Whitechurch H. 1991. Hydrothermal activity inthe Lau back-arcbasin: Sulfides and water chemistry. Geology, 19.. 303～306.
|
| [20] | Gu Lianxin, Xu Keqin. 1987. The tectonic development and relatedmetallogenesis ofthe Lower Yangtze fault depression belt. Journalof Guilin College of Geology, 7(4)： 243～251 (in Chinese withEnglish abstract).
|
| [21] | Gu Lianxin, Xu Keqin. 1986. On the South China type massive sulfideore depositsformed in marine fault depression troughs on the continental crust. Mineral Deposits, 5(2) . 1 ～ 13 (in Chinese withEnglish abstract).
|
| [22] | Gu Lianxin, He Jinxiang, Hu Wenxuan, Xu Keqin. 1997. Effect ofcrustal maturity onore composition of massive sulphide deposits inSouth China. Acta Geologica Sinica, 71(2):161～169 (in Chinese with English abstract). Krebs W. 1981. The geology of theMeggen oredeposit. in: Wolf K H. ed. Handbook of stratabound and stratiform ore deposits, Vol. 9.Amsterdam: ElsevierScientific Publishing Company, 509 ～ 550.
|
| [23] | Marchig V, Gundlach H, Moller P and Schley F. 1982. Some geochemical indicatorsfor discrimination between diagenetic and hydrothermal metalliferrous sediments. MarineGeology, 50: 241～256.
|
| [24] | Meylan M A, Glasby G P, Knedler K E. and Johnston J H. 1981.Metalliferous deep-seasediments. in: Wolf K H. ed. Handbookof strata-bound and stratiform ore deposits, Vol. 9.Amsterdam:Elsevier Scientific Publishing Company, 77～178.
|
| [25] | Miao Yuanxing, Ran Congying. 1992. Geological and geochemicalcharacteristics ofdongshengmiao Pb-Zn-S Deposit of submarineexhalative origin, Inner Mongolia. Geochimica,21 (4): 375～383(in Chinese with English abstract).
|
| [26] | Smith P A, Cronan D S. 1983. The geochemistry of metalliferous sediments andwaters associated with shallow submarine hydrothermal activity (Santorini, Aegean Sea).Chemical Geology, 39:241～262.
|
| [27] | Tu Guangchi. 1988. Geochemistry of the stratabound deposit in China(Vol. 3).Beijing: Geological Publishing House. 152～ 168 (inChinese).
|
| [28] | Wang Ziqiang, Zhang Linghua, Zhou Hongrui, Xu Bei. 1990. Tectonic development ofthe southeastern and the northern continental margins of the Yangtze Platform in theMiddle and Late Proterozoic. in: Wang Hongzhen, Yang Sennan, Liu Benpei, et al.eds.Tectonopalaeogeography and palaeobiogeography of Chinaand adjacient Regions. Wuhan: Pressof the China University ofGeosciences, 246～264 (in Chinese).
|
| [29] | Wei Heming. 1990. The submarine exhalative mineralization types andtheir spatialdistribution in the Fengxian-Taibai Pb-Zn ore fieldin the Qinling Mountains. GeologicalReview, 36 (5): 394 ～ 403(in Chinese with English abstract).
|
| [30] | Zhou Yongzhang. 1990. On sedimentary geochemistry of siliceousrocks originatedfrom thermal water in Nandan-Hechi Basin.Acta Sedimentologica Sinica, 8(3): 75～83(inChinese with English abstract).
|
| [31] | 毕治国,王贤方,朱鸿等.1988.皖南震旦系.见：地层古生物论文集(第19辑).北京：地质出版社.27～54.
|
| [32] | 陈多福,陈先沛.1992.广西德保泥盆系硅岩的沉积特征和成因探讨.地球化学,21(2)：190～197.
|
| [33] | 陈多福,陈光谦,潘晶铭等.1998.广东云浮大降坪超大型黄铁矿矿床的热水沉积特征.地球化学,27(1)：12～18.
|
| [34] | 顾连兴,徐克勤.1986.论大陆地壳断裂拗陷带中的华南型块状硫化物矿床.矿床地质,5(2)：1～13.
|
| [35] | 顾连兴,徐克勤.1987.长江中、下游断裂拗陷带的构造发展与成矿作用.桂林冶金地质学院学报,7(4)：243～251.
|
| [36] | 刘英俊,曹励明,李兆麟等.1984.元素地球化学.北京：科学出版社.77～85.
|
| [37] | 谢窦克,张宗清.1989.东南沿海基底杂岩的同位素年代学研究.中国地质科学院南京地质矿产研究所所刊,10(3)：24～34.
|
| [38] | 杨松生.1989.皖南浙西地区多金属矿成矿条件浅析.地质与勘探,(5)：13～17.
|
| [39] | 周永章.1990.丹池盆地热水成因硅岩的沉积地球化学特征.沉积学报,8(3)：75～83.
|
| [40] | Large D E. 1981. Sediment-hosted submarine exhalative lead-zinc deposits-review oftheir geological characteristics and genesis. in:Wolf K H. ed. Handbook of strata-boundand stratiform ore deposits, Vol. 9. Amsterdam: Elsevier Scientific Publishing Company,469～508.
|
| [41] | Li Jianzhong, He Dianren, Wu Jianmin. 1992. The Qinling-type leadand zinc oredeposit. Acta Geologica Sinica, 66 ( 3 ): 257 ～ 268 (inChinese with English abstract).
|
| [42] | Li Shuangying, Yan Hualxue, Jin Fuquan. 1993. Geochemical characteris of anoxicenvironment of the Upper Sinian Lantian Formation in South Anhui. Geology of Anhui,3(3):16～21 (inChinese).
|
| [43] | Li Shuangying. 1998. The discovery of hydrothermal deposits in Lantian Formation,Upper Smian in the Southern Anhui and its Significance. Geology of Anhui, 8(4): 7～10(inChinese).
|
| [44] | Liu Yingjun, Cao Liming, Li Zhaolin, Wang Henian, Chu Tongqing,Zhang Jingrong.1984. Geochemistry of individual elements. Beijing.. Science Press. 77～85 (in Chinese).
|
| [45] | Xie Douke, Zhang Zongqing, Shang Yuqiang, Jiang Chuanren. 1989.Isotopicgeochronologic study of basement complex in Southeastcoast of China. Bulletin of theNanjing Institute of Geology andMineral Resources, Chinese Academy of Geological Sciences,10(3) :24～34 (in Chinese with English abstract).
|
| [46] | Xing Fengming, Xu Xiang, Chen Jiangfeng, Zou Taixi, Forland K A.1992. The LateProterozoic continental accretionary history of thesoutheastern margin of the Yangtzeplatform. Acta GeologicaSinica, 66(1): 59～72 (in Chinese with English abstract).
|
| [47] | Yang Songsheng. 1989. A perliminary analysis on metallogenetic conditions ofpolymetallic ore deposits in Southern Anhui-WesternZhejiang Area. Geology and Prospecting,5: 13～ 17 (in Chinesewith English abstract).
|
