安徽沿江地区晚石炭世黄龙组白云岩地球化学特征及其成因研究

赵大千, 李双应, 王冰, 嵇在飞, 芦艳琳, 孟祥金, 吕庆田. 安徽沿江地区晚石炭世黄龙组白云岩地球化学特征及其成因研究[J]. 地质科学, 2012, 47(3): 851-866.
引用本文: 赵大千, 李双应, 王冰, 嵇在飞, 芦艳琳, 孟祥金, 吕庆田. 安徽沿江地区晚石炭世黄龙组白云岩地球化学特征及其成因研究[J]. 地质科学, 2012, 47(3): 851-866.
Zhao Daqian, Li Shuangying, Wang Bing, Ji Zaifei, Lu Yanlin, Meng Xiangjin, Lü Qingtian. Geochemistry characteristics and origin of Upper Carboniferous Huanglong Formation dolomites in the Anhui segment of the Lower Yangtze area[J]. Chinese Journal of Geology, 2012, 47(3): 851-866.
Citation: Zhao Daqian, Li Shuangying, Wang Bing, Ji Zaifei, Lu Yanlin, Meng Xiangjin, Lü Qingtian. Geochemistry characteristics and origin of Upper Carboniferous Huanglong Formation dolomites in the Anhui segment of the Lower Yangtze area[J]. Chinese Journal of Geology, 2012, 47(3): 851-866.

安徽沿江地区晚石炭世黄龙组白云岩地球化学特征及其成因研究

详细信息
    作者简介:

    赵大千, 男, 1986年6月生,硕士研究生,沉积地质学和地层学专业。E-mail: zhaodaqian419@163.com

    通讯作者: 李双应, 男, 1956年9月生,博士,教授,沉积地质学和地层学专业。 E-mail: lsystevsen@126.com
  • 中图分类号: P534.45, P588.245

Geochemistry characteristics and origin of Upper Carboniferous Huanglong Formation dolomites in the Anhui segment of the Lower Yangtze area

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    Corresponding author: Li Shuangying
  • 安徽沿江地区晚石炭世黄龙组白云岩广泛发育,主要为晶粒白云岩,其次是角砾白云岩和残余颗粒白云岩。地球化学分析表明,安徽沿江地区黄龙组白云岩中Fe、Mn、Sr、Na含量分别为:2 567×10-6(1 600×10-6~4 400×10-6)、353×10-6(166×10-6~742×10-6)、109.7×10-6(69.0×10-6~176.5×10-6)、288×10-6(100×10-6~700×10-6),稀土元素总量为7.29×10-6(2.56×10-6~20.82×10-6),ΣLREE/ΣHREE比值平均为3.07(1.16~10.17),经海水标准化后,显示LREE富集,HREE相对亏损,δCe平均为4.53(2.82~7.78),正异常显著,δEu平均为1.85(0.94~2.92),配分模式曲线显示白云岩化流体来自海水。白云岩中可见蒸发岩类或蒸发构造。综合分析认为该地区白云岩主要为准同生成因,部分为埋藏成岩成因,其中角砾白云岩为准同生成因,怀宁地区白云岩δEu平均为2.38(1.91~2.92),正异常显著,表明后期受到热液流体影响。
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  • [1]

    常印佛,刘湘培,吴言昌.1991.长江中下游铜铁成矿带.北京:地质出版社.1-379.

    [2]

    Chang Yinfo,Liu Xiangpei and Wu Yanchang.1991.The Copper and Iron Ore Belt in the Middle and Lower Yangtze.Beijing:Geology Publishing House.1-379.

    [3]

    陈永权,周新源,杨海军.2010.塔里木盆地塔中地区上寒武统3种截面特征白云岩的岩石地球化学特征与成因研究.沉积学报, 28 (2): 209-218.

    [4]

    Chen Yongquan,Zhou Xinyuan and Yang Haijun.2010.Geochemical research and genesis of dolostones with different crystal characteristics occurring in the Upper Cambrian,central area of Tarim Basin.Acta Sedimentologica Sinica, 28 (2): 209-218.

    [5]

    洪天求,李双应,胡永强.2000.安徽铜陵地区石炭系层序地层研究.合肥工业大学学报(自然科学版), 23 (3): 299-303.

    [6]

    Hong Tianqiu,Li Shuangying and Hu Yongqiang.2000.The study of sequence stratigraphy of Upper Carboniferous series in the area of Tongling,Anhui.Journal of Hefei University of Technology(Natural Science), 23 (3): 299-303.

    [7]

    胡文瑄,陈 琪,王小林,曹 剑.2010.白云岩储层形成演化过程中不同流体作用的稀土元素判别模式.石油与天然气地质, 31 (6): 810-818.

    [8]

    Hu Wenxuan,Chen Qi,Wang Xiaolin and Cao Jian.2010.REE models for the discrimination of fluids in the formation and evolution of dolomite reservoirs.Oil & Gas Geology, 31 (6): 810-818.

    [9]

    李双应,金福全.1994.下扬子盆地石炭纪的岩石学特征及沉积相.安徽地质, 4 (3): 36-47.

    [10]

    Li Shuangying and Jin Fuquan.1994.Carboniferous petrographic features and depositional facies of the Lower Yangtze Basin.Geology of Anhui, 4 (3): 36-47.

    [11]

    李双应.2000.LYB石炭系碳酸盐岩微量元素地球化学特征.合肥工业大学学报(自然科学版), 23 (5): 654-659.

    [12]

    Li Shuangying.2000.The geochemical characteristics of trace elements in Carboniferous carbonate rocks in Lower Yangtze Basin.Journal of Hefei University of Technology(Natural Science), 23 (5): 654-659.

    [13]

    杨秋荣,王金芳,冯景志,侯增谦,杨竹森,蒙义峰,王聪颖,陈文韬.2010.安徽铜陵天马山金硫矿床地质地球化学特征.地球学报, 31 (2): 203-208.

    [14]

    Yang Qiurong,Wang Jinfang,Feng Jingzhi,Hou Zengqian,Yang Zhusen,Meng Yifeng,Wang Congying and Chen Wentao.2010.Geological and geochemical characteristics of the Tianmashan Au-S deposit in Tongling,Anhui Province.Acta Geoscientica Sinica, 31 (2): 203-208.

    [15]

    黄成刚,黄思静,吴素娟,陈启林.2006.100 Ma来海水的锶同位素组成演化及主要控制因素.地球科学与环境学报, 28 (2): 19-24.

    [16]

    Huang Chenggang,Huang Sijing,Wu Sujuan and Chen Qilin.2006.Sr-isotope composition and evolvement in sea water over past 100 Ma and control factors.Journal of Earth Sciences and Environment, 28 (2): 19-24.

    [17]

    王小林,金之钧,胡文瑄,张军涛,钱一雄,朱井泉,李 庆.2009.塔里木盆地下古生界白云石微区REE配分特征及其成因研究.中国科学(D辑), 39 (6): 721-733.

    [18]

    Wang Xiaolin,Jin Zhijun, Hu Wenxuan,Zhang Juntao,Qian Yixiong, Zhu Jingquan and Li Qing.2009.Using in situ REE analysis to study the origin and diagenesis of dolomite of Lower Paleozoic,Tarim Basin.Science in China(Series D), 52 (5): 681-693.

    [19]

    汪建国,陈代钊,严德天,韦恒叶,遇 昊.2011.湘西地区前寒武纪-寒武纪转折期碳酸盐-硅泥质沉积体系的截然转换:地层-沉积样式|形成机理及意义.地质科学, 46 (1):27-41.

    [20]

    Wang Jianguo,Chen Daizhao,Yan Detian, Wei Hengye and Yu Hao.2011. Sharp transition from carbonates to cherts across the platform margin in western Hunan,south China during precambrian-Cambrian transition: Stratal-depositional patterns,mechanisms and implications.Chinese Journal of Geology, 46 (1):27-41.

    [21]

    张 瑛,陈宏明,汤再如.1984.老虎洞白云岩的成因特征.资源调查与环境, 5 (1): 67-80.

    [22]

    Zhang Ying,Chen Hongming and Tang Zairu.1984.Some genetic characteristics of Laohudong dolomite.Resources Survey & Environment, 5 (1): 67-80.

    [23]

    Adams J E and Rhodes M L.1960.Dolomitization by seepage refluxion.AAPG Bulletin, 44 (12): 1912-1920.

    [24]

    Badiozamani K.1973.The dorag dolomitization model,application to the Middle Ordovician of Wisconsin.Journal of Sedimentary Research, 43 (4): 965-984.

    [25]

    Baker P A and Burns S J.1985.Occurrence and formation of dolomite in organic-rich continental margin sediments.AAPG Bulletin, 69 (11): 1917-1930.

    [26]

    Banner J L,Hanson G N and Meyers W J.1988.Rare earth element and Nd isotopic variations in regionally extensive dolomites from the Burlington-Keokuk Formation(Mississippian); implications for REE mobility during carbonate diagenesis.Sedimentary Petrology, 58 (3): 415-432.

    [27]

    Bau M and Dulski P. 1996. Distribution of yttrium and rare-earth elements in the Penge and Kuruman iron-formations, Transvaal Supergroup, south Africa. Precambrian Research, 79 (1-2):37-55.

    [28]

    Boynton W V.1984.Geochemistry of the rare earth elements: Meteorite studies.In:Henderson P(Ed.).Rare Earth Element Geochemistry.Amsteram: Elservier.63-114.

    [29]

    Brand U and Veizer J.1980.Chemical diagenesis of a multi-component carbonate system; 1,trace elements.Journal of Sedimentary Research, 50 (4): 1219-1236.

    [30]

    Carballo J D,Land L S and Miser D E.1987.Holocene dolomitization of supratidal sediments by active tidal pumping,Sugarloaf Key,Florida.Journal of Sedimentary Research, 57 (1): 153-165.

    [31]

    Compton J S.1988.Degree of supersaturation and precipitation of organogenic dolomite.Geology, 16 (4): 318-321.

    [32]

    Davies G R and Smith J L B. 2006. Structurally controlled hydrothermal dolomite reservoir facies: An overview. AAPG Bulletin, 90 (11):1641-1690.

    [33]

    Douville E,Bienvenu P,Charlou J L,Donval J P,Fouquet Y,Appriou P and Gamo T.1999.Yttrium and rare earth elements in fluids from various deep-sea hrdrothermal systems.Geochimica et Cosmochimica Acta, 63 (5): 627-643.

    [34]

    Feng Z Z and Jin Z K.1994.Types and origin of dolostones in the Lower Palaeozoic of the North China Platform.Sedimentary Geology, 93 (3-4): 279-290.

    [35]

    Hsü K J and Siegenthaler C.1969.Preliminary experiments on hydrodynamic movement induced by evaporation and their bearing on the dolomite problem.Sedimentology, 12 (1-2): 11-25.

    [36]

    James R H and Elderfield H.1996.Chemistry of ore-forming fluids and mineral formation rates in an active hydrothermal sulfide deposit on the Mid-Atlantic Ridge.Geology, 24 (12): 1147-1150.

    [37]

    Kawabe Ⅰ,Torium T,Ohta A and Miura N.1998.Monoisotopic REE abundances in seawater and the origin of seawater tetrad effect.Geochemical Journal, 32: 213-229.

    [38]

    Land L S.1985.The origin of massive dolomite.Journal of Geological Education, 33: 112-125.

    [39]

    Land L S and Hoops G K.1973.Sodium in carbonate sediments and rocks; a possible index to the salinity of diagenetic solutions.Journal of Sedimentary Research, 43 (3): 614-617.

    [40]

    Machel H G and Lonnee J.2002.Hydrothermal dolomite--A product of poor definition and imagination.Sedimentary Geology, 152 (3-4): 163-171.

    [41]

    Mclennan S M.1989.Rare earth elements in sedimentary rocks influence of provenance and sedimentary processes.Reviews in Mineralogy and Geochemistry, 21 (1): 169-200.

    [42]

    Michard A,Albarede F,Michard G Minster J F and Charlou J L.1983.Rare-earth elements and uranium in high-temperature solutions from East Pacific Rise hydrothermal vent field (13°N).Nature, 303: 795-797.

    [43]

    Middleton K,Coniglio M,Sherlock R and Frape S K.1993.Dolomitization of Middle Ordovician carbonate reservoirs,southwestern Ontario.Bulletin of Canadian Petroleum Geology, 41 (2): 150-163.

    [44]

    Miura N,Asahara Y and Kawabe Ⅰ.2004.Rare earth element and Sr isotopic study of the Middle Permian limestone-dolostone sequence in Kuzuu area,central Japan: Seawater tetrad effect and Sr isotopic signatures of seamount-type carbonate rocks.The Journal of Earth and Planetary Sciences,Nagoya University, 51: 11-35.

    [45]

    Piper D Z.1974.Rare earth elements in the sedimentary cycle: A summary.Chemical Geology, 14 (4): 285-304.

    [46]

    Qing H R and Mountjoy E W.1994.Rare earth element geochemistry of dolomites in the Middle Devonian Presqu'ile barrier,western Canada sedimentary basin: Implications for fluid-rock ratios during dolomitization.Sedimentology, 41 (4): 787-804.

    [47]

    Sun S Q.1995.Dolomite reservoirs porosity evolution and reservoir characteristics.AAPG Bulletin, 79 (2): 186-204.

    [48]

    Taylor S R,Mclennan S M,Armstrong R L and Tarney J.1981.The composition and evolution of the continental crust:Rare earth element evidence from sedimentary rocks.Philosophical Transactions of the Royal Society A, 301 (1461): 381-399.

    [49]

    Wallace M W.1990.Origin of dolomitization on the Barbwire Terrace,Canning Basin,western Australia.Sedimentology, 37 (1): 105-122.

    [50]

    Walker G,Abumere O E and Kamaluddin B.1989.Luminescence spectroscope of Mn2+ centres in rock-forming carbonates.Mineralogical Magazine, 53 (370): 201-211.

    [51]

    Warren J.2000.Dolomite: Occurrence,evolution and economically important associations.Earth Science Reviews, 52 (1-3): 1-81.

    [52]

    Webb G E and Kamber B S.2000.Rare earth elements in Holocene reefal microbialites: A new shallow seawater proxy.Geochimica et Cosmochimica Acta, 64 (9): 1557-1565.

    [53]

    Zenger D H,Dunham J B and Ethington R L.1980.Concepts and Models of Dolomitization.Society of Economic Paleontologists and Mineralogists,Special Publication.Tulsa,Okla: The Society.1-320.

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出版历程
收稿日期:  2012-02-10
修回日期:  2012-04-18
刊出日期:  2012-07-25

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