大别造山带东缘韧性剪切带中构造岩的构造地球化学分析
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摘要
安徽省桐城市挂镇(挂车河镇)地区出露郯庐断裂系(北北东—北东向)和大别构造系(近东西向)的韧性剪切带,变质温度分别为400℃~450℃和600℃~700℃,均发育镁铁质和长英质构造岩,是研究不同变形条件下岩石中元素活化迁移规律的理想对象。质量平衡计算表明长英质剪切带在韧性变形过程中,大别构造系体积基本不变,郯庐断裂系体积亏损且随变形程度的增强而增加;镁铁质性剪切带在脆—韧变形过程中体积增加。长英质构造岩的稀土和微量元素变异远弱于镁铁质构造岩,长英质构造岩基本继承了原岩的特征而镁铁质构造岩与原岩的差异显著,长英质和镁铁质混合的构造岩主要显示镁铁质组分的迁移规律。长英质构造岩的元素迁移种类和迁移率与变形程度和变质温度正相关,其中体积亏损变形的郯庐断裂系表现为重稀土中等迁出、中稀土几乎未迁移和轻稀土微弱迁入;等体积变形的大别构造系为稀土元素迁入,轻稀土、中稀土和重稀土的迁移率依次增加。镁铁质构造岩的稀土元素迁移表现为轻稀土强烈迁入和重稀土中等迁出。体积变化不是元素变异的主因;在原岩和矿物蚀变制约的基础上,元素迁移受到岩石流变分异作用和热液渗流作用的双重作用,低温时以渗透流体作用为主,而高温时岩石流变分异作用增强。
The Tanlu fault joins the Dabie orogenic belt on its eastern margin.There are ductile shear zones of NNE-NE trending of Tanlu fault system and EW trending of Dabie tectonic system in Guazhen(or Guachehe town) area,Tongcheng city,Anhui Province.Those ductile shear zones of two tectonic systems,which are ideal to research element migration in different deformation conditions,both develop mafic and felsic tectonites with deformation temperature of 400℃~450℃ and 600℃~700℃ respectively.Mass balance calculations suggest that volumes of felsic shear zones in Dabie tectonic system were almost constant while volume-loss of felsic shear zones in Tanlu fault system increased with the deformation intensity during ductile deformation,and mafic shear zones gained in volume during brittle-ductile deformation.The variations of REEs and trace elements in felsic tectonites were far lower than that of mafic teetonites,the former on the whole inherited chief feature of host rocks while the latter were remarkably different with that of host rocks.Under mix of mafic and felsic components,tectonite would mostly reveal the element migration features of mafic component.The kinds and rates of element migration in felsic rocks were positive correlation with intensity and temperature of the ductile shearing deformation.Therein,HREEs,MREEs and LREEs of volume-loss Tanlu fault system were respectively medium losses,little/no change and little gains,while REEs gains of isovolume Dabie tectonic system in turn increased from LREEs,MREEs to HREEs.In mafic tectonites,LREEs were largely gains and HREEs were medium losses.The volume loss is not the real reason for variation of REEs and trace elements in the shear zone.Based on restriction of host rocks and mineral alteration,the joint function of rock rheological differentiation and fluid filtration with high water/rock ratio is the predominant reason for element migration,and the latter was predominant under lower deformation temperature while the former was enhanced with increment of deformation temperature.
The Tanlu fault joins the Dabie orogenic belt on its eastern margin.There are ductile shear zones of NNE-NE trending of Tanlu fault system and EW trending of Dabie tectonic system in Guazhen(or Guachehe town) area,Tongcheng city,Anhui Province.Those ductile shear zones of two tectonic systems,which are ideal to research element migration in different deformation conditions,both develop mafic and felsic tectonites with deformation temperature of 400℃~450℃ and 600℃~700℃ respectively.Mass balance calculations suggest that volumes of felsic shear zones in Dabie tectonic system were almost constant while volume-loss of felsic shear zones in Tanlu fault system increased with the deformation intensity during ductile deformation,and mafic shear zones gained in volume during brittle-ductile deformation.The variations of REEs and trace elements in felsic tectonites were far lower than that of mafic teetonites,the former on the whole inherited chief feature of host rocks while the latter were remarkably different with that of host rocks.Under mix of mafic and felsic components,tectonite would mostly reveal the element migration features of mafic component.The kinds and rates of element migration in felsic rocks were positive correlation with intensity and temperature of the ductile shearing deformation.Therein,HREEs,MREEs and LREEs of volume-loss Tanlu fault system were respectively medium losses,little/no change and little gains,while REEs gains of isovolume Dabie tectonic system in turn increased from LREEs,MREEs to HREEs.In mafic tectonites,LREEs were largely gains and HREEs were medium losses.The volume loss is not the real reason for variation of REEs and trace elements in the shear zone.Based on restriction of host rocks and mineral alteration,the joint function of rock rheological differentiation and fluid filtration with high water/rock ratio is the predominant reason for element migration,and the latter was predominant under lower deformation temperature while the former was enhanced with increment of deformation temperature.
引文
高利娥,曾令森,胡明月等,2011.榴辉岩韧性剪切变形中的流体作用及地球化学效应.岩石学报,27(4):1095—1115.Gao Li'e,Zeng Lingsen,Hu Mingyue et al.2011.Nature and geochemical effects of fluids during ductile shearing of UHP eclogite.Acta Petrologica Sinica,27(4):1095—1115.
李振生,田晓莉,张文俊等.2013.安徽桐城挂车河镇地区东西向韧性剪切带分形特征及其估算应变速率适用性分析.科技导报,31(20):15—19.Li Zhensheng,Tian Xiaoli,Zhang Wenjun et al.2013.Foetal analysis of east-west ductile shear zone in Guachehe town area,Tongeheng,Anhui and its applicability of strain-rate estimation.Science&Technology Review,31(20):15—19.
林伟,王清晨,石永红.2005.大别山—苏鲁碰撞造山带构造几何学、运动学和岩石变形分析.岩石学报,21(4):1195—1214.Lin Wei,Wang Qingchen and Shi Yonghong.2005.Arcllitecture,kinematics and deformation analysis in Dabie-Sulu collision zone.Acta Petrologica Sinica,21(4):1195—1214.
刘德良,扬晓勇,杨海涛等.1996.郯庐断裂带南段桴槎山韧性剪切带糜棱岩的变形条件和组分迁移系.岩石学报,12(4):573—588.Liu Deliang,Yang Xiaoyong,Yang Haitao et al.1996.The deformatlonal condition and component migration of mylonites in Fuchashan ductile shear zones in the southern Tanchen-Lujiang fanlt belt.Acts Petrologica Sinica,12(4):573—588.
吕古贤,孙岩,刘德良等.2011.构造地球化学的回顾与展望.大地构造与成矿学,35(4):479—494.L(u|¨)Guxian,Sun Yon,Liu Deliang et al.2011.Tectono-geochemistry:A review.Geotectonica et Metallogenia,35(4):479—494.
骆文娟,张德会.2009.韧性剪切带中稀土元素变异原因新探——对体积亏损公式解释剪切体系中稀土变异的讨论及稀土变异的若干原因.地质与资源,18(3):189—196.Luo Wenjuan and Zhang Dehui.2009.A new exploration to the rare earth element variations in ductile shear zone:Discussion on the volume Ioss formula and reasons for REE variation.Geology and Resources,18(3):189—196.
彭渤,刘翔.1998.沉积变质岩系中:REE断裂构造地球化学.大地构造与成矿学,22(1):75—81.Peng Be and Liu Xiang.1998.REE geochemical characteristics of faults developed in sedimentary-metamorphic rocks.Geotectonica et Metallogenia,22(1):73—81.
戚学祥,许志琴,齐金忠.2006.苏鲁地体南部南岗—高公岛韧性剪切带的变形记录、组分迁移和体积亏损.地质学报,80(12):1939—1947.Qi Xuexiang,Xu Zhiqin and Qi Jinzhong.2006.Deformational record,compositional variation and volume loss for the Nan guang-Gaogongdao ductile shear zone in the southern Sulu terrane.Acts Geologica Sinica,80(12):1939—1947.
宋传中,张华,任升莲等.2011.长江中下游转换构造结与区域成矿背景分析.地质学报,85(5):778—788.Song Chuanzhong,Zhang Hua,lien Shenglian et al.2011.Transform tectonic node of the middle and lower reaches of the Yangtze River and analysis of regional metallogenic settings.Acts Geologiea Sinica,85(5):778—788.
孙岩,徐士进,刘德良等.1998.断裂构造地球化学导论.北京:科学出版社.1—246.Sun Yan,Xu Shijin,Liu Deliang et al.1998.Introduction to Fault Tectonogeochemistry.Beijing:Science Press.1—246.
索书田,钟增球,游振东.2000.大别地块超高压变质期后伸展变形及超高压变质岩石折返过程.中国科学(D辑),30(1):9—17.Sue Shutian,Zhong Zengqiu and You Zhendong.2000.Extensional deformation of post ultrahigh-pressure metamorphism and exhumation process of ultrabigh-pressure metamorphic rocks in the Dabie massif,China.Seisnce in China(Series D),43(3):225—236.
谭秋明,刘忠明.1995.新城—黄陂走滑韧性剪切带的动力分异作用.大地构造与成矿学,19(2):171—177.Tan Qiuming and Liu Zhongming.1995.Dynamic differentiation of Xincheng-Huangpi right-lateral ductile shear zone.Geotectonica et Metallogenia,19(2):171—177.
汤加富,周存亭,侯明金等.2003.大别山及邻区地质构造特征与形成演化:地幔差速环流与陆内多期造山.jE京:地质出版社.1—266.Tang Jiafu,Zhou Cunting,Hou Mingjin et al.2003.The Geological Characteristics,Formation and Evolution of Dabie Mountains and Its Adjacent Regions.Beijing:Geological Publishing House.1—266.
王勇生,朱光,王道轩等.2004..大别山东缘郯庐两期走滑剪切带形成的温压条件与造山带折返的关系.大地构造与成矿学,28(3):228—238.Wang Yongsheng,Zhu Guang,Wang Daoxuan et al.2004.Relation between P-T contitions of two phases of Tan-Lu strike-slip shear zones and delamination of the orogenic belts on the eastern margin of the Dabie Mountains.Geotectonica et Metallogenia,28(3):228—238.
吴维平,徐树桐,江来利等.2000.大别山东部桐城挂镇地区超高压变质杂岩的变形历史.安徽地质,10(3):199—204.Wu Weiping,Xu Shutong,Jiang Laili et al.2000.The deformation history of the ultrahigh pressure metamorphic(UHPM)complex in the Guazhen area,tongcheng,eastern Dabie Mountains.Geology of Anhui,10(3):199—204.
杨凤根,王鹤年,华仁民.2004.河台金矿中稀土元素在韧性剪切过程中迁移行为的研究.中国稀土学报,22(1):164—170.Yang Fenggnn,Wang Henian and Hua Renmin.2004.Transportation of REE in ductile shear zone in Hetai gold deposit.Journal of the Chinese Rare Earth Society,22(1):164—170.
杨晓勇,刘德良,戴晓平等.1999.韧性剪切变形条件下花岗岩中稀土元素变化特征研究.稀土,20(1):6—10.Yang Xiaoyong,Liu Deliang,Dai Xiaoping et al.1999.Study of REE variations of granite and its deformed tectonic rocks under ductile shearing.Chinese Rare Earths,20(1):6—10.
杨晓勇.2005.论韧性剪切带研究及其地质意义.地球科学进展,20(7):765—771.Yang Xiaoyong.2005.On the studies of ductile shear zones:Their geological significance.Advances in Earth Science,20(7):765—771.
杨新岳,谢国源,李志纯等.1995.变形过程中的流体——岩石作用和变形岩石质量平衡.中国科学(B辑),25(3):329—336.Yang Xinyue,Xie Guoyuan,Li Zhichun et al.1995.Fluid-rock interaction and mass balance of deformed rock in deformation Taking the Eritx tectonic zone,northern Xinjiang.Science in China(Series B),38(7):865—875.
杨元根,吴学益,金志升等.2004.海南二甲金矿的动力变形成矿作用及构造地球化学模拟实验研究.大地构造与成矿学,28(3):320—329.Yang Yuangen,Wu Xueyi,Jin Zhisheng et al.2004.Dynamic deformation related ore-forming process and tectono-geochemical simulating experiments of Erjia gold deposit,Hainan Province.Geotectonica et Metallogenia,28(3):320—329.
曾令森,李海兵,许志琴等.2004.混合岩中浅色体的有限迁移及其对变形分解的影响.地质学报,78(6):752—757.Zeng Lingsen,Li Haibing,Xu Zhiqin et al.2004.Limited of leucosome in a migmatite and effects of progressive partial reel ring on strain partitioning.Acts Geologica Sinica,78(6):752—757.
张文俊,李振生,田晓莉等.2012.安徽桐城挂车河镇地区韧性剪切带元素质量平衡分析.安徽地质,22(4):241—247.Zhang Wenjun,Li Zhensheng,Tian Xiaoli et al.2012.Element and mass balance analysis of ductile shear zone in the Guachehe town area,Tongcheng,Anhui.Geology of Anhui,22(4):241—247.
钟增球,游振东.1995.剪切带的成分变异及体积亏损——以河台剪切带为例.科学通报,40(10):913—916.Zhong Zengqiu and You Zhendong.1995.Compositional variation and volume loss of a shear zone Hetai shear zone as a case history.Chinese Science Bulletin,40(19):1638—1641.
周建波,胡克,洪景鹏.1999.稀土元素在韧性剪切带体积亏损研究中的应用——以胶南造山带构造岩为例.地质论评,45(3):24l一246.Zhou Jianbo,Hu Ke and Hong Jingpeng,1999.Application of REE anomaly in volume deficiency of a ductile shear zone:An example from the ductile shear zone on the northern margin of the Jiaonan orogenic belt.Geological Review.45(3):241—246.
朱光,刘国生,Dunlap W J等.2004.郯庐断裂带同造山走滑运动的~(40)Ar/~(39)Ar年代学证据.科学通报,49(2):190—198.Zhu Guang,Liu Guosheng,Dunlap W Jet al.2004.~(40)Ar/~(39)Ar geochronological constraints on syn-orogenic strike-slip movement of Tan-Lu fault zone.Chinese Science Bulletin,49(5):499—508.
朱光,张力,谢成龙等.2009.郯庐断裂带构造演化的同位素年代学制约.地质科学,44(4):1327—1342.Zhu Guang,Zhang Li,Xie Chenglong et al.2009.Geochronological constraints on tectonic evolution of the Tan-Lu fault zone.Chinese Journal of Geology,44(4):1327—1342.
Ague J J.1991.Evidence for major mass transfer and volume strain during regional metamorphism of pelites.Geology,19(8):855—858.
Alderton D H M,Pearee J A and Ports P J,1980.Rare earth element mobility during granite alteration:Evidence from Southwest England.Earth and Planetary Science Letters,49(1):149—165.
Ban M.1991.Rare-earth element mobility during hydrothermal and metamorphic fluid-rack interaction and the significance of the oxidation state of europium.Chemical Geology,93(3—4):219—230.
Boynton W V.1984.Cosmochemistry of the rare earth elements:Meteorite studies.In:Henderson P(Ed.),Rare Earth Element Geochemistry(Developments in Geochemistry,Volume 2),Amstenlam:Elseriver.63—114,
Byrne R H and Kim K-H.1993.Rare earth precipitation and coprecipitation behavior:The limiting role of PO_4~(3-)on dissolved rare earth concentrations in seawater.Geochimics et Cosmochimiea Acts,$7(3):519—526.
Campbell I H,Lesher C M,Coad Pet al.1984.Rare-earth element mobility in alteration pipes below massive Cu Zn-sulfide deposits.Chemical Geology,45(3—4):181—202.
Chen J and Wang H.1994.Distribution of REE and other trace elements in the Hetai gold deposit of South China:Implications for evolution of an auriferous shear zone.Journal of Southeast Asian Earth Sciences,10(3—4):217—226.
Condie K C and Sinha A K.1996.Rare earth and other trace element mobility during mylonitization:A comparison of the Brevard and Hope Valley shear zones in the Appalachian Mountains,USA.Journal of Metamorphic Geology,14(2):213—226.
Cullers R L,Medaris L G and Haskin L A.1973.Experimental studies of the distribution of rare earths as trace elements among silicate minerals and liquids and water.Geochimica et Cosmochimica Acts,37(6):1499—1512,
Davisen I,McCarthy M,Powell D et al.1995.Laminar flow in shear zones:The Pernambuco shear zone,NE-Brazil.Journal of Structural Geology,17(2):149—161.
Dipple G M,Wintsch R P and Andrews M S.1990.Identification of the scales of differential element mobility in a ductile fault zone.Journal of Metamorphic Geology,8(6):645—661.
Faure M,Lin W,Seharer U etal.2003.Continental subduction and exhumation of UHP rocks:Structural and geochronological insights from the Dahieshan(East China).Lithos,70(3—4):213—241.
Glazner A F and Bartley J M.1991.Volume loss,fluid flow and state of strain in extensional mylonites from the central Mojave Desert,California.Journal of Structural Geology,13(5):587—594.
Grant J A.1986.The isocon diagram:A simple solution to Gresena'equation for metaaomatic alteration.Economic Geology,81(8):1976—1982.
Grant J A.2005.Isocon analysis:A brief review of the method and applications.Physics and Chemistry of the Esrth,30(17—18):997—1004.
Handy M R.1990.The solid-state flow of polymineralic rocks.Journal of Geophysical Research,95(B6):8647—8661.
Handy M R,Wissing S B and Streit L E.1999.Frictional-viscous flow in mylonite with varied bimineralic composition and its effect on lithospheric strength.Teetonophysics,303(1—4):175—191.
Hopf S.1993.Behaviour of rare earth elements in geothermal systems of New Zealand.journal of Geochemical Exploration,47(1—3):333—357.
Jonasson R G,Bancroft G M and Nesbitt H W.1985.Solubihties of some hydrous REE phosphates with implications for diagenesis and sea water concentrations.Geochimica et Cosmochimica Acta,49(10):2133—2139.
Kwon S,Park Y,Park C et al.2009.Mass-balance analysis of bulk-rock chemical changes during mylenitizatien of a megacrystbearing granitoid,Cheongsan shear zone,Korea.Journal of Asian Earth Sciences,35(6):489—501.
Leroy J L and Turpin L.1988.REE,Th and U behaviour during hydrothermal and supergene processes in a granitic environment.Chemical Geology,68(3—4):239—251.
Li B L,Shu L S,Sun Y et al.2001.Experimental analysis of ductile-slip rhealogy in shallow structural level faults.Science in China(Series D),44(6):481—489.
Liu X and Byrne R H.1997.Rare earth and yttrium phosphate solubilities in aqueous solution.Geochimica et Cosmachimica Acta,61(8):1625—1633.
Ludden J N and Thompson G.1979.An evaluation of the behavior of the rare earth elements during the weathering of sea-floor basalt.Earth and Planetary Science Letters,43(1):85—92.
MacLean W H.1988.Rare earth element mobility at constant inter-REE ratios in the alteration zone at the Phelps Dodge massive sulphide deposit,Matagami,Quebec.Mineralium Deposita,23(4):231—238.
Michibayashi K.1996.The role of intragranular fracturing on grain size reduction in feldspar during mylonitization.Journal of Structural Geology,18(1):17—25.
Middelburg J J,Van Der Weijden C H and Woittiez J R W.1988.Chemical processes affecting the mobility of major,minor and trace elements during weathering of granitic rocks.Chemical Geology,liB(3—4):253—273.
Nabelek P I.1987.General equations for modeling fluid/rock interaction using trace elements and isotopes.Geochimica et Cosmochimica Acta,51(6):1765—1769.
Newman J and Mitra G.i993.Lateral variations in mylonite zone thickness as influenced by fluid-rock interactions,Linville falls fault,North Carolina.Journal of Structural Geology,15(7):849—863.
O'Hara K.1988.Fluid flow and valume loss during mylonitization:An origin for phyllonite in an overthrnst setting,North Carolina U.S.A.Tectonophysics,156(1—2):21—36.
O'Hara K and Blackburn W H.1989.Valume-loss modal for trace-element enrichments in mylonites.Geology,17(6):524—527.
O'Hara K D.1994.Fluid-reek interaction in ernstal shear zones:A directed pereelation appreaeh.Geology,22(9):843—846.
Olsen S N and Grant J A.1991.Isoeon analysis of migmatisation in the Front Range,Colorado,USA.Journal of Metamorphic Geology,9(2):151—164.
Ratschbacher L,Hacker B R,Webb L E et al.2000.Exhumation of the ultrahigh-pressure continental crust in east central China:Cretaceous and Cenozoic unroofing and the Tan-Lu fault.Journat of Geophysical Research,105(B6):13303—13338.
Rollinsan H R.1993.Using Geochemical Data:Evaluation,Presentation,Interpretation.New York:Longman Scientific&Technical.1—352.
Seifert K E and Chadima S A.1989.Depletion of heavy rare-earth elements in metamorphic minerals from Adirondack anorthosites.Geology,17(11):1004—1006.
Selverstone J,Morteani G and Staude J M.1991.Fluid channelling during ductile shearing:Transformation of granodiorite,into aluminous schist in the Tauern Window,eastern Alps.Journal of Metamorphic Geology,9(4):419—431.
St(a|¨)hle H J,Raith M,Hoernes S et al.1987.Element mobility during incipient granulite formation at Kabbaldurga,southern India.Journal of Petrology,28(5):803—834.
Sun Y,Shen X and Liu$.1984.Preliminary analysis of some chemically determined data from the compressive fault zone at Dayu,Jiangxi Province.Geochemistry,3(3):285—294.
Sun Y,Shu L S,Guo J C et al.2003.Teetono-geoehemistry analyses of fault recks in shear zone of metamorphic core complex in North Jiangxi,China.Progress in Natural Science,13(5):363—373.
Thompson R N.1982.Magmatism of the Bristish Tertiary volcanic previnee.Scottish Journal of Geology,18(1):49—107.
Tobisch O T,Barton M D,Vernon R H et al.1991.Fluid-enhanced deformation:Transformation of granitoids to banded mylonitas,western Sierra Nevada,California,and southeastern Australia.Journal of Structural Geology,13(10):1137—1156.
Wickham S M.1987.The segregation and emplacement of granitic magmas.Journal of the Geological Society,144(2):281—297.
Winchester J A and Max M D.1984.Element mobility associated with syn-metamorphic shear zones near Seotehport,NW Mayo,Ireland.Journal of Metamorphic Geology,2(1):1—11.
Wood D A,Gibson I L and Thompson R N.1976.Elemental mobility during zeolite facies metamorphism of the Tertiary basalts of eastern Iceland.Contributions to Mineralogy and Petrology,55(3):241—254.
Xiang B W,Wang Y S,Li C C et al.2008.Evolution of the Xiaotian-Mozitan fault and its implications for exhumation of Dabie HP-UHP rocks.Progress in Natural Science,18(6):713—722.
Xiong Y L and Zhai Y S.1991.The mobility of rare-earth elements during hydrothermal activity:A review.Chinese Journal of Geochemistry,10(4):295—306.
Zhu W B,Sun Y,Guo J C et al.2003.Prespects for study of teetono-geoehemistry.Progress in Natural Science,13(3):161—165.
Zhu G,Wang Y,Liu G et al.2005.~(40)Ar/~(39)Ar dating of strike-slip motion on the Tan-Lu fault zone,East China.Journal of Structural Geology,27(8):1379—1398.
Zhu G,Liu G S,Niu M L et al.2009.Syn-collisional transform faulting of the Tan-Lu fault zone,East China.International Journal of Earth Sciences,98(1):135—155.
李振生,田晓莉,张文俊等.2013.安徽桐城挂车河镇地区东西向韧性剪切带分形特征及其估算应变速率适用性分析.科技导报,31(20):15—19.Li Zhensheng,Tian Xiaoli,Zhang Wenjun et al.2013.Foetal analysis of east-west ductile shear zone in Guachehe town area,Tongeheng,Anhui and its applicability of strain-rate estimation.Science&Technology Review,31(20):15—19.
林伟,王清晨,石永红.2005.大别山—苏鲁碰撞造山带构造几何学、运动学和岩石变形分析.岩石学报,21(4):1195—1214.Lin Wei,Wang Qingchen and Shi Yonghong.2005.Arcllitecture,kinematics and deformation analysis in Dabie-Sulu collision zone.Acta Petrologica Sinica,21(4):1195—1214.
刘德良,扬晓勇,杨海涛等.1996.郯庐断裂带南段桴槎山韧性剪切带糜棱岩的变形条件和组分迁移系.岩石学报,12(4):573—588.Liu Deliang,Yang Xiaoyong,Yang Haitao et al.1996.The deformatlonal condition and component migration of mylonites in Fuchashan ductile shear zones in the southern Tanchen-Lujiang fanlt belt.Acts Petrologica Sinica,12(4):573—588.
吕古贤,孙岩,刘德良等.2011.构造地球化学的回顾与展望.大地构造与成矿学,35(4):479—494.L(u|¨)Guxian,Sun Yon,Liu Deliang et al.2011.Tectono-geochemistry:A review.Geotectonica et Metallogenia,35(4):479—494.
骆文娟,张德会.2009.韧性剪切带中稀土元素变异原因新探——对体积亏损公式解释剪切体系中稀土变异的讨论及稀土变异的若干原因.地质与资源,18(3):189—196.Luo Wenjuan and Zhang Dehui.2009.A new exploration to the rare earth element variations in ductile shear zone:Discussion on the volume Ioss formula and reasons for REE variation.Geology and Resources,18(3):189—196.
彭渤,刘翔.1998.沉积变质岩系中:REE断裂构造地球化学.大地构造与成矿学,22(1):75—81.Peng Be and Liu Xiang.1998.REE geochemical characteristics of faults developed in sedimentary-metamorphic rocks.Geotectonica et Metallogenia,22(1):73—81.
戚学祥,许志琴,齐金忠.2006.苏鲁地体南部南岗—高公岛韧性剪切带的变形记录、组分迁移和体积亏损.地质学报,80(12):1939—1947.Qi Xuexiang,Xu Zhiqin and Qi Jinzhong.2006.Deformational record,compositional variation and volume loss for the Nan guang-Gaogongdao ductile shear zone in the southern Sulu terrane.Acts Geologica Sinica,80(12):1939—1947.
宋传中,张华,任升莲等.2011.长江中下游转换构造结与区域成矿背景分析.地质学报,85(5):778—788.Song Chuanzhong,Zhang Hua,lien Shenglian et al.2011.Transform tectonic node of the middle and lower reaches of the Yangtze River and analysis of regional metallogenic settings.Acts Geologiea Sinica,85(5):778—788.
孙岩,徐士进,刘德良等.1998.断裂构造地球化学导论.北京:科学出版社.1—246.Sun Yan,Xu Shijin,Liu Deliang et al.1998.Introduction to Fault Tectonogeochemistry.Beijing:Science Press.1—246.
索书田,钟增球,游振东.2000.大别地块超高压变质期后伸展变形及超高压变质岩石折返过程.中国科学(D辑),30(1):9—17.Sue Shutian,Zhong Zengqiu and You Zhendong.2000.Extensional deformation of post ultrahigh-pressure metamorphism and exhumation process of ultrabigh-pressure metamorphic rocks in the Dabie massif,China.Seisnce in China(Series D),43(3):225—236.
谭秋明,刘忠明.1995.新城—黄陂走滑韧性剪切带的动力分异作用.大地构造与成矿学,19(2):171—177.Tan Qiuming and Liu Zhongming.1995.Dynamic differentiation of Xincheng-Huangpi right-lateral ductile shear zone.Geotectonica et Metallogenia,19(2):171—177.
汤加富,周存亭,侯明金等.2003.大别山及邻区地质构造特征与形成演化:地幔差速环流与陆内多期造山.jE京:地质出版社.1—266.Tang Jiafu,Zhou Cunting,Hou Mingjin et al.2003.The Geological Characteristics,Formation and Evolution of Dabie Mountains and Its Adjacent Regions.Beijing:Geological Publishing House.1—266.
王勇生,朱光,王道轩等.2004..大别山东缘郯庐两期走滑剪切带形成的温压条件与造山带折返的关系.大地构造与成矿学,28(3):228—238.Wang Yongsheng,Zhu Guang,Wang Daoxuan et al.2004.Relation between P-T contitions of two phases of Tan-Lu strike-slip shear zones and delamination of the orogenic belts on the eastern margin of the Dabie Mountains.Geotectonica et Metallogenia,28(3):228—238.
吴维平,徐树桐,江来利等.2000.大别山东部桐城挂镇地区超高压变质杂岩的变形历史.安徽地质,10(3):199—204.Wu Weiping,Xu Shutong,Jiang Laili et al.2000.The deformation history of the ultrahigh pressure metamorphic(UHPM)complex in the Guazhen area,tongcheng,eastern Dabie Mountains.Geology of Anhui,10(3):199—204.
杨凤根,王鹤年,华仁民.2004.河台金矿中稀土元素在韧性剪切过程中迁移行为的研究.中国稀土学报,22(1):164—170.Yang Fenggnn,Wang Henian and Hua Renmin.2004.Transportation of REE in ductile shear zone in Hetai gold deposit.Journal of the Chinese Rare Earth Society,22(1):164—170.
杨晓勇,刘德良,戴晓平等.1999.韧性剪切变形条件下花岗岩中稀土元素变化特征研究.稀土,20(1):6—10.Yang Xiaoyong,Liu Deliang,Dai Xiaoping et al.1999.Study of REE variations of granite and its deformed tectonic rocks under ductile shearing.Chinese Rare Earths,20(1):6—10.
杨晓勇.2005.论韧性剪切带研究及其地质意义.地球科学进展,20(7):765—771.Yang Xiaoyong.2005.On the studies of ductile shear zones:Their geological significance.Advances in Earth Science,20(7):765—771.
杨新岳,谢国源,李志纯等.1995.变形过程中的流体——岩石作用和变形岩石质量平衡.中国科学(B辑),25(3):329—336.Yang Xinyue,Xie Guoyuan,Li Zhichun et al.1995.Fluid-rock interaction and mass balance of deformed rock in deformation Taking the Eritx tectonic zone,northern Xinjiang.Science in China(Series B),38(7):865—875.
杨元根,吴学益,金志升等.2004.海南二甲金矿的动力变形成矿作用及构造地球化学模拟实验研究.大地构造与成矿学,28(3):320—329.Yang Yuangen,Wu Xueyi,Jin Zhisheng et al.2004.Dynamic deformation related ore-forming process and tectono-geochemical simulating experiments of Erjia gold deposit,Hainan Province.Geotectonica et Metallogenia,28(3):320—329.
曾令森,李海兵,许志琴等.2004.混合岩中浅色体的有限迁移及其对变形分解的影响.地质学报,78(6):752—757.Zeng Lingsen,Li Haibing,Xu Zhiqin et al.2004.Limited of leucosome in a migmatite and effects of progressive partial reel ring on strain partitioning.Acts Geologica Sinica,78(6):752—757.
张文俊,李振生,田晓莉等.2012.安徽桐城挂车河镇地区韧性剪切带元素质量平衡分析.安徽地质,22(4):241—247.Zhang Wenjun,Li Zhensheng,Tian Xiaoli et al.2012.Element and mass balance analysis of ductile shear zone in the Guachehe town area,Tongcheng,Anhui.Geology of Anhui,22(4):241—247.
钟增球,游振东.1995.剪切带的成分变异及体积亏损——以河台剪切带为例.科学通报,40(10):913—916.Zhong Zengqiu and You Zhendong.1995.Compositional variation and volume loss of a shear zone Hetai shear zone as a case history.Chinese Science Bulletin,40(19):1638—1641.
周建波,胡克,洪景鹏.1999.稀土元素在韧性剪切带体积亏损研究中的应用——以胶南造山带构造岩为例.地质论评,45(3):24l一246.Zhou Jianbo,Hu Ke and Hong Jingpeng,1999.Application of REE anomaly in volume deficiency of a ductile shear zone:An example from the ductile shear zone on the northern margin of the Jiaonan orogenic belt.Geological Review.45(3):241—246.
朱光,刘国生,Dunlap W J等.2004.郯庐断裂带同造山走滑运动的~(40)Ar/~(39)Ar年代学证据.科学通报,49(2):190—198.Zhu Guang,Liu Guosheng,Dunlap W Jet al.2004.~(40)Ar/~(39)Ar geochronological constraints on syn-orogenic strike-slip movement of Tan-Lu fault zone.Chinese Science Bulletin,49(5):499—508.
朱光,张力,谢成龙等.2009.郯庐断裂带构造演化的同位素年代学制约.地质科学,44(4):1327—1342.Zhu Guang,Zhang Li,Xie Chenglong et al.2009.Geochronological constraints on tectonic evolution of the Tan-Lu fault zone.Chinese Journal of Geology,44(4):1327—1342.
Ague J J.1991.Evidence for major mass transfer and volume strain during regional metamorphism of pelites.Geology,19(8):855—858.
Alderton D H M,Pearee J A and Ports P J,1980.Rare earth element mobility during granite alteration:Evidence from Southwest England.Earth and Planetary Science Letters,49(1):149—165.
Ban M.1991.Rare-earth element mobility during hydrothermal and metamorphic fluid-rack interaction and the significance of the oxidation state of europium.Chemical Geology,93(3—4):219—230.
Boynton W V.1984.Cosmochemistry of the rare earth elements:Meteorite studies.In:Henderson P(Ed.),Rare Earth Element Geochemistry(Developments in Geochemistry,Volume 2),Amstenlam:Elseriver.63—114,
Byrne R H and Kim K-H.1993.Rare earth precipitation and coprecipitation behavior:The limiting role of PO_4~(3-)on dissolved rare earth concentrations in seawater.Geochimics et Cosmochimiea Acts,$7(3):519—526.
Campbell I H,Lesher C M,Coad Pet al.1984.Rare-earth element mobility in alteration pipes below massive Cu Zn-sulfide deposits.Chemical Geology,45(3—4):181—202.
Chen J and Wang H.1994.Distribution of REE and other trace elements in the Hetai gold deposit of South China:Implications for evolution of an auriferous shear zone.Journal of Southeast Asian Earth Sciences,10(3—4):217—226.
Condie K C and Sinha A K.1996.Rare earth and other trace element mobility during mylonitization:A comparison of the Brevard and Hope Valley shear zones in the Appalachian Mountains,USA.Journal of Metamorphic Geology,14(2):213—226.
Cullers R L,Medaris L G and Haskin L A.1973.Experimental studies of the distribution of rare earths as trace elements among silicate minerals and liquids and water.Geochimica et Cosmochimica Acts,37(6):1499—1512,
Davisen I,McCarthy M,Powell D et al.1995.Laminar flow in shear zones:The Pernambuco shear zone,NE-Brazil.Journal of Structural Geology,17(2):149—161.
Dipple G M,Wintsch R P and Andrews M S.1990.Identification of the scales of differential element mobility in a ductile fault zone.Journal of Metamorphic Geology,8(6):645—661.
Faure M,Lin W,Seharer U etal.2003.Continental subduction and exhumation of UHP rocks:Structural and geochronological insights from the Dahieshan(East China).Lithos,70(3—4):213—241.
Glazner A F and Bartley J M.1991.Volume loss,fluid flow and state of strain in extensional mylonites from the central Mojave Desert,California.Journal of Structural Geology,13(5):587—594.
Grant J A.1986.The isocon diagram:A simple solution to Gresena'equation for metaaomatic alteration.Economic Geology,81(8):1976—1982.
Grant J A.2005.Isocon analysis:A brief review of the method and applications.Physics and Chemistry of the Esrth,30(17—18):997—1004.
Handy M R.1990.The solid-state flow of polymineralic rocks.Journal of Geophysical Research,95(B6):8647—8661.
Handy M R,Wissing S B and Streit L E.1999.Frictional-viscous flow in mylonite with varied bimineralic composition and its effect on lithospheric strength.Teetonophysics,303(1—4):175—191.
Hopf S.1993.Behaviour of rare earth elements in geothermal systems of New Zealand.journal of Geochemical Exploration,47(1—3):333—357.
Jonasson R G,Bancroft G M and Nesbitt H W.1985.Solubihties of some hydrous REE phosphates with implications for diagenesis and sea water concentrations.Geochimica et Cosmochimica Acta,49(10):2133—2139.
Kwon S,Park Y,Park C et al.2009.Mass-balance analysis of bulk-rock chemical changes during mylenitizatien of a megacrystbearing granitoid,Cheongsan shear zone,Korea.Journal of Asian Earth Sciences,35(6):489—501.
Leroy J L and Turpin L.1988.REE,Th and U behaviour during hydrothermal and supergene processes in a granitic environment.Chemical Geology,68(3—4):239—251.
Li B L,Shu L S,Sun Y et al.2001.Experimental analysis of ductile-slip rhealogy in shallow structural level faults.Science in China(Series D),44(6):481—489.
Liu X and Byrne R H.1997.Rare earth and yttrium phosphate solubilities in aqueous solution.Geochimica et Cosmachimica Acta,61(8):1625—1633.
Ludden J N and Thompson G.1979.An evaluation of the behavior of the rare earth elements during the weathering of sea-floor basalt.Earth and Planetary Science Letters,43(1):85—92.
MacLean W H.1988.Rare earth element mobility at constant inter-REE ratios in the alteration zone at the Phelps Dodge massive sulphide deposit,Matagami,Quebec.Mineralium Deposita,23(4):231—238.
Michibayashi K.1996.The role of intragranular fracturing on grain size reduction in feldspar during mylonitization.Journal of Structural Geology,18(1):17—25.
Middelburg J J,Van Der Weijden C H and Woittiez J R W.1988.Chemical processes affecting the mobility of major,minor and trace elements during weathering of granitic rocks.Chemical Geology,liB(3—4):253—273.
Nabelek P I.1987.General equations for modeling fluid/rock interaction using trace elements and isotopes.Geochimica et Cosmochimica Acta,51(6):1765—1769.
Newman J and Mitra G.i993.Lateral variations in mylonite zone thickness as influenced by fluid-rock interactions,Linville falls fault,North Carolina.Journal of Structural Geology,15(7):849—863.
O'Hara K.1988.Fluid flow and valume loss during mylonitization:An origin for phyllonite in an overthrnst setting,North Carolina U.S.A.Tectonophysics,156(1—2):21—36.
O'Hara K and Blackburn W H.1989.Valume-loss modal for trace-element enrichments in mylonites.Geology,17(6):524—527.
O'Hara K D.1994.Fluid-reek interaction in ernstal shear zones:A directed pereelation appreaeh.Geology,22(9):843—846.
Olsen S N and Grant J A.1991.Isoeon analysis of migmatisation in the Front Range,Colorado,USA.Journal of Metamorphic Geology,9(2):151—164.
Ratschbacher L,Hacker B R,Webb L E et al.2000.Exhumation of the ultrahigh-pressure continental crust in east central China:Cretaceous and Cenozoic unroofing and the Tan-Lu fault.Journat of Geophysical Research,105(B6):13303—13338.
Rollinsan H R.1993.Using Geochemical Data:Evaluation,Presentation,Interpretation.New York:Longman Scientific&Technical.1—352.
Seifert K E and Chadima S A.1989.Depletion of heavy rare-earth elements in metamorphic minerals from Adirondack anorthosites.Geology,17(11):1004—1006.
Selverstone J,Morteani G and Staude J M.1991.Fluid channelling during ductile shearing:Transformation of granodiorite,into aluminous schist in the Tauern Window,eastern Alps.Journal of Metamorphic Geology,9(4):419—431.
St(a|¨)hle H J,Raith M,Hoernes S et al.1987.Element mobility during incipient granulite formation at Kabbaldurga,southern India.Journal of Petrology,28(5):803—834.
Sun Y,Shen X and Liu$.1984.Preliminary analysis of some chemically determined data from the compressive fault zone at Dayu,Jiangxi Province.Geochemistry,3(3):285—294.
Sun Y,Shu L S,Guo J C et al.2003.Teetono-geoehemistry analyses of fault recks in shear zone of metamorphic core complex in North Jiangxi,China.Progress in Natural Science,13(5):363—373.
Thompson R N.1982.Magmatism of the Bristish Tertiary volcanic previnee.Scottish Journal of Geology,18(1):49—107.
Tobisch O T,Barton M D,Vernon R H et al.1991.Fluid-enhanced deformation:Transformation of granitoids to banded mylonitas,western Sierra Nevada,California,and southeastern Australia.Journal of Structural Geology,13(10):1137—1156.
Wickham S M.1987.The segregation and emplacement of granitic magmas.Journal of the Geological Society,144(2):281—297.
Winchester J A and Max M D.1984.Element mobility associated with syn-metamorphic shear zones near Seotehport,NW Mayo,Ireland.Journal of Metamorphic Geology,2(1):1—11.
Wood D A,Gibson I L and Thompson R N.1976.Elemental mobility during zeolite facies metamorphism of the Tertiary basalts of eastern Iceland.Contributions to Mineralogy and Petrology,55(3):241—254.
Xiang B W,Wang Y S,Li C C et al.2008.Evolution of the Xiaotian-Mozitan fault and its implications for exhumation of Dabie HP-UHP rocks.Progress in Natural Science,18(6):713—722.
Xiong Y L and Zhai Y S.1991.The mobility of rare-earth elements during hydrothermal activity:A review.Chinese Journal of Geochemistry,10(4):295—306.
Zhu W B,Sun Y,Guo J C et al.2003.Prespects for study of teetono-geoehemistry.Progress in Natural Science,13(3):161—165.
Zhu G,Wang Y,Liu G et al.2005.~(40)Ar/~(39)Ar dating of strike-slip motion on the Tan-Lu fault zone,East China.Journal of Structural Geology,27(8):1379—1398.
Zhu G,Liu G S,Niu M L et al.2009.Syn-collisional transform faulting of the Tan-Lu fault zone,East China.International Journal of Earth Sciences,98(1):135—155.