江南造山带东段璜茅-五城-屯溪韧性剪切带塑性变形及流变学研究
|
摘要
江南造山带东段皖赣相邻区璜茅-五城-屯溪韧性剪切带野外现象、室内显微构造特征表明其经历了较为强烈的韧性剪切变形。岩石经历了NNE向右行剪切改造,变质变形程度为初糜棱岩-糜棱岩阶段,少量达超糜棱岩阶段。结合石英普遍发育边界迁移重结晶、长石多以塑性拉长和少量膨凸重结晶的变形行为特征、石英C轴组构显示出中-高温柱面和菱面滑移为主、重结晶石英颗粒大小-频数及分形维数(1.1646～1.2007),Kruhl温度计测算,揭示了璜茅-五城-屯溪韧性剪切带以中高温位错蠕变变形为主,变形和糜棱岩化环境在450～600℃的中深地壳范围,相当于中高绿片岩相-低角闪岩相。同时,岩石变形的古差异应力为20.76～30.04 MPa,估算所得应变速率主要介于10~(-14)～10~(-11) s~(-1),指示了中高温、低应变速率的韧性变形条件。已有的变形年龄显示,该韧性剪切带为加里东构造事件产物,主要的动力来源与江山-绍兴断裂带发育的陆内俯冲作用主应力在远离造山带的转变相关。
The Huangmao-Wucheng-Tunxi ductile shear zone, which is located in the eastern segment of the Jiangnan orogenic belt, is characterized by intensive ductile shear deformation as shown by its field appearance and the microstructures. The rocks were metamorphosed and deformed as protomylonite to mylonite, and locally as ultramylonite due to the NNE trending right-lateral ductile shearing. The quartz grains mostly occur as dynamic recrystallization including subgrain rotation and grain boundary migration recrystallization. Meanwhile, most of feldspar porphyroclasts are enlongated and some are fully bulging recrystallized. Quartz C-axis fabric demonstrates that quartz fabrics are mainly middle-high temperature prismatic slip system and low-middle temperature rhomb slip system. The size of quartz recrystallized particles is mainly 20 to 140 μm. Fractal analysis suggests that the fractal dimension of boundaries of the recrystallized quartz grains is 1.1646 to 1.2007. All above characteristics reveal that the deformation type of this ductile shear zone belongs to dislocation creep at middle-high temperature. The calculation of the Kruhl thermometer with fractal method indicates that the ductile deformation and mylonitization temperatures range from 400 to 600 ℃, which is equivalent to the metamorphic conditions of middle-high greenschist facies to lower amphibolite facies. In addition, the differential stress and strain rate of the ductile shear zone are estimated at 20.76 to 30.04 MPa, 10~(-14) to 10~(-11) s~(-1), which indicates that the ductile deformation condition is medium-high temperature and low strain rate. Because the deformation is believed to take place in the Caledonian, we therefore suggest that the geodynamics of this ductile shear zone is related to transition of the principal stress that is remotely affected by the Caledonian intracontinental subduction along the Jiangshan-Shaoxing fault zone.
The Huangmao-Wucheng-Tunxi ductile shear zone, which is located in the eastern segment of the Jiangnan orogenic belt, is characterized by intensive ductile shear deformation as shown by its field appearance and the microstructures. The rocks were metamorphosed and deformed as protomylonite to mylonite, and locally as ultramylonite due to the NNE trending right-lateral ductile shearing. The quartz grains mostly occur as dynamic recrystallization including subgrain rotation and grain boundary migration recrystallization. Meanwhile, most of feldspar porphyroclasts are enlongated and some are fully bulging recrystallized. Quartz C-axis fabric demonstrates that quartz fabrics are mainly middle-high temperature prismatic slip system and low-middle temperature rhomb slip system. The size of quartz recrystallized particles is mainly 20 to 140 μm. Fractal analysis suggests that the fractal dimension of boundaries of the recrystallized quartz grains is 1.1646 to 1.2007. All above characteristics reveal that the deformation type of this ductile shear zone belongs to dislocation creep at middle-high temperature. The calculation of the Kruhl thermometer with fractal method indicates that the ductile deformation and mylonitization temperatures range from 400 to 600 ℃, which is equivalent to the metamorphic conditions of middle-high greenschist facies to lower amphibolite facies. In addition, the differential stress and strain rate of the ductile shear zone are estimated at 20.76 to 30.04 MPa, 10~(-14) to 10~(-11) s~(-1), which indicates that the ductile deformation condition is medium-high temperature and low strain rate. Because the deformation is believed to take place in the Caledonian, we therefore suggest that the geodynamics of this ductile shear zone is related to transition of the principal stress that is remotely affected by the Caledonian intracontinental subduction along the Jiangshan-Shaoxing fault zone.
引文
邓国辉,罗春林,楼法生,廖六根,凌联海.2002.德兴?黄山断裂带及其邻区的地质研究进展.资源调查与环境,23(4):250-256.
段留安,杨晓勇,孙卫东.2010.皖南天井山?小贺金矿区地质地球化学特征及找矿前景分析.矿床地质,29(S1):921-922.
段留安,杨晓勇,孙卫东,方世明,余良范,范增平.2011.皖南天井山金矿床地质?地球化学特征及找矿前景.地质学报,85(6):965-978.
高林志,丁孝忠,曹茜,张传恒.2010.中国晚前寒武纪年表和年代地层序列.中国地质,37(4):1014-1020.
高林志,杨明桂,丁孝忠,刘燕学,刘训,凌联海,张传恒.2008.华南双桥山群和河上镇群凝灰岩中的锆石SHRIMP U-Pb年龄--对江南新元古代造山带演化的制约.地质通报,27(10):1744-1751.
胡玲,刘俊来,纪沫,曹淑云,张宏远,张忠岩.2009.变形显微构造识别手册.北京:地质出版社:1-96.
黄学猛,张进江,许志琴.2016.电子背散射衍射(EBSD)技术在地壳构造变形研究中的应用.地质学报,90(6):1130-1145.
李建波,王涛,郭磊,童英,欧阳志侠,曾涛,史兴俊,张建军.2012.韧性剪切带的剪切作用类型和韧性减薄量.地质通报,31(1):26-37.
李婧,刘永江,李伟民,金巍,梁琛岳,温泉波,张媛媛.2016.华北克拉通基底花岗质片麻岩变形和流变学研究--以辽西寺儿堡地区为例.大地构造与成矿学,40(5):891-907.
李小兵,裴先治,陈有炘,刘成军,李佐臣,李瑞保,陈国超,魏博.2015.东昆仑造山带东段哈图沟-清水泉-沟里韧性剪切带塑性变形及动力学条件研究.大地构造与成矿学,39(2):208-230.
梁琛岳,刘永江,孟婧瑶,温泉波,李伟民,赵英利,米晓楠,张丽.2015.舒兰韧性剪切带应变分析及石英动态重结晶颗粒分形特征与流变参数估算.地球科学,40(1):116-129.
刘俊来,曹淑云,邹运鑫,宋志杰.2008.岩石电子背散射衍射(EBSD)组构分析及应用.地质通报,27(10):1638-1645.
覃有晃,林南孙,王爱国.1990.安徽省歙县?休宁地区金矿成矿地质条件及成矿预测研究报告.安徽省地质矿产局332地质队.
舒良树,于津海,贾东,王博,沈渭洲,张岳桥.2008.华南东段早古生代造山带研究.地质通报,27(10):1581-1593.
王德恩,韩守玉,杨荷金.2003.安徽省休宁县山斗金矿天井山矿段详查地质报告.安徽省地质矿产局332地质队.
王积善,张均.2016.皖南天井山地区金矿与韧性剪切带的关系.矿业工程研究,31(2):65-69.
王积善,张均,王健.2016.皖南天井山地区大型韧性剪切带特征及EBSD石英组构分析.矿物岩石,36(1):96-105.
王强,赵振华,简平,许继峰,包志伟,马金龙.2004.德兴花岗闪长斑岩SHRIMP锆石U-Pb年代学和Nd-Sr同位素地球化学.岩石学报,20(2):315-324.
王新社,郑亚东,杨崇辉,侯贵廷.2001.用动态重结晶石英颗粒的分形确定变形温度及应变速率.岩石矿物学杂志,20(1):36-41.
王勇,余达淦,管太阳,刘平辉,巫建华.2002.赣东北地区早白垩世火山岩的岩石学及岩石化学特征.岩石矿物学杂志,21(1):31-40.
汪明辉.2017.皖南地区金矿类型与成矿地质条件剖析.资源信息与工程,32(1):32-33.
吴建阳,张均.2010.从天井山金矿和金山金矿的成矿特征对比谈天井山金矿的找矿前景及突破方向.矿床地质,29(S1):1003-1004.
吴荣新,郑永飞,吴元保.2005a.皖南新元古代花岗闪长岩体锆石U-Pb定年以及元素和氧同位素地球化学研究.岩石学报,21(3):587-606.
吴荣新,郑永飞,吴元保.2005b.皖南石耳山新元古代花岗岩锆石U-Pb定年以及元素和氧同位素地球化学研究.高校地质学报,11(3):364-382.
吴荣新,郑永飞,吴元保.2007.皖南新元古代井潭组火山岩锆石U-Pb定年和同位素地球化学研究.高校地质学报,13(2):282-296.
夏浩然,刘俊来.2011.石英结晶学优选与应用.地质通报,30(1):58-60.
向必伟,朱光,王勇生,谢成龙,胡召齐.2007.糜棱岩化过程中矿物变形温度计.地球科学进展,22(2):126-134.
许志琴,王勤,梁凤华,陈方远,徐翠萍.2009.电子背散射衍射(EBSD)技术在大陆动力学研究中的应用.岩石学报,25(7):1721-1736.
徐海军,金淑燕,郑伯让.2007.岩石组构学研究的最新技术--电子背散射衍射(EBSD).现代地质,21(2):213-225.
徐先兵,汤帅,林寿发.2016.赣北景德镇韧性剪切带两类剪切指向及其构造意义.高校地质学报,22(2):308-316.
薛怀民,马芳,宋永勤,谢亚平.2010.江南造山带东段新元古代花岗岩组合的年代学和地球化学:对扬子与华夏地块拼合时间与过程的约束.岩石学报,26(11):3215-3244.
薛怀民,汪应庚,马芳,汪诚,王德恩,左延龙.2009.皖南太平?黄山复合岩体的SHRIMP年代学:由钙碱性向碱性转变对扬子克拉通东南部中生代岩石圈减薄时间的约束.中国科学(D辑),39(7):979-993.
杨昔林,曹殿华,李以科,黄玉凤,阚迎松,刘盛祥.2011.江西德兴孔家?银山火山盆地的时代归属:锆石U-Pb年代学证据.中国地质,38(1):86-108.
余心起,江来利,许卫,邱瑞龙,杜建国,戴圣潜.2007.皖浙赣断裂带的界定及其基本特征.地学前缘,14(3):102-13.
俞云文,徐步台,陈江峰,董传万.2001.浙东南中生代晚期火山岩Nd同位素组成及其地层学意义.高校地质学报,7(1):62-69.
张秉良,刘瑞珣,向宏发,楚全芝,黄雄南,郑勇刚.2008.红河断裂带中南段糜棱岩分形特征及主要流变参数的估算.地震地质,30(2):473-483.
张波,张进江,郭磊.2006.北喜马拉雅穹隆带然巴韧性剪切带石英动态重结晶颗粒的分维几何分析与主要流变参数的估算.地质科学,41(1):158-169.
张彦杰,周效华,廖圣兵,张晓东,武彬,王存智,余明刚.2010.皖赣鄣公山地区新元古代地壳组成及造山过程.地质学报,84(10):1401-1427.
赵崇贺,何科昭,邰道乾,乐昌硕,聂泽同.1997.赣东北地区重要火成岩的40Ar/39Ar年龄.地球科学,22(3):257-260.
郑蕾,周永章,曾长育.2013.钦杭结合带(南段)庞西垌断裂中动态重结晶石英颗粒分形特征及主要流变参数估算.中山大学学报(自然科学版),52(2):106-114.
周涛发,袁峰,侯明金,杜建国,范裕,朱光,岳书仓.2004.江南隆起带东段皖赣相邻区燕山期花岗岩类的成因及形成的地球动力学背景.矿物岩石,24(3):65-71.
周翔,余心起,王德恩,张德会,李春麟,傅建真,董会明.2011.皖南东源含W、Mo花岗闪长斑岩及成矿年代学研究.现代地质,25(2):201-210.
Bailey C M and Eyster E L.2003.General shear deformation in the Pinaleno Mountains metamorphic core complex,Arizona.Journal Structural Geology,25(11):1883-1893.
Boutonnet E,Leloup P H,Sassier C,Gardien V and Ricard Y.2013.Ductile strain rate measurements document long-term strain localization in the continental crust.Geology,41(8):819-822.
Charvet J,Shu L S,Shi Y S,Guo L Z and Faure M.1996.The building of south China:Collision of Yangzi and Cathaysia blocks,problems and tentative answers.Journal of Asian Sciences,13(3-5):223-235.
Chu Y and Lin W.2014.Phanerozoic polyorogenic deformation in southern Jiuling massif,northern South China block:Constraints from structural analysis and geochronology.Journal of Asian Sciences,86(3):117-130.
Faure M,Shu L,Wang B,Charvet J,Choulet F and MoniéP.2009.Intracontinental subduction:A possible mechanism for the Early Palaeozoic Orogen of SE China.Terra Nova,21(5):360-368.
Hacker B R,Yin A,Christie J M and Snoke A W.1990.Differential stress,strain rate,and temperatures of mylonitization in the Ruby Mountains,Nevada:Implications for the rate and duration of uplift.Journal of Geophysical Research,95(B6):8569-8580.
Hirth G,Teyssier C and Dunlap W J.2001.An evaluation of quartzite flow laws based on comparisons between experimentally and naturally deformed rocks.International Journal of Earth Sciences,90(1):77-87.
Hirth G and Tullis J.1992.Dislocation creep regimes in quartz aggregates.Journal of Structural Geology,14(2):145-159.
Hirth G and Tullis J.1994.The brittle-plastic transition in experimentally deformed quartz aggregates.Journal of Geophysical Research Solid Earth,99(B6):11731-11747.
Jessup M J,Cottle J M,Newell D L,Searle M P,Law R Dand Tracy R J.2006.Vorticity of flow and dis-placement along the South Tibetan Detachment System,Gondasampa region,Tibet.Journal of Asian Earth Sciences,26:143.
Ji S C,Jiang Z T,Rybacki E,Wirth R,Prior D and Xia B,2004.Strain softening and microstructural evolution of anorthite aggregates and quartz-anorthite layered composites deformed in torsion.Earth and Planetary Science Letters,222(2):377-390.
Ji S C and Mainprice D.1987.Experimental deformation of sintered above and below the order-disorder transition.Geodinamica Acta,1(2):113-124.
Ji S C and Mainprice D.1988.Natural deformation fabrics of plagioclase:Implications for slip systems and seismic anisotropy.Tectonophysics,147(1):145-163.
Ji S C and Mainprice D.1990.Recrystallization and fabric development in plagioclase.Journal of Geology,98(1):65-79.
Ji S C,Rybacki E,Wirth R,Jiang Z T and Xia B.2005.Mechanical and microstructural characterization of calcium aluminosilicate(CAS)and Si O2/CAS composites deformed at high temperature and high pressure.Journal of the European Ceramic Society,25(4):301-311.
Koch P S.1983.Rheology and microstructures of experimentally deformed quartz aggregates.Los Angeles:Ph D Dissertation,University of California:1-464.
Koch P S,Christie J M,Ord A and George R P.1989.Effect of water on the rheology of experimentally deformed quartzite.Journal of Geophysical Research Solid Earth,94(B10):13975-13996.
Kruhl J H and Nega M.1996.The fractal shape of sutured quartz grain boundaries:Application as a geothermometer.Geologische Rundschau,85(1):38-43.
Kruhl J H,Nega M and Milla H E.1995.The Fractal Shape of Grain Boundary Sutures:Reality,Model and Application as a Geothermometer//Book of Abstracts,2nd International Conference on Fractal and Dynamic Systems in Geosciences,84:31-32.
Kurz W,Fritz H,Tenczer V and Unzog W.2002.Tectonometamorphic evolution of the Koralm Complex(Eastern Alps):Constrains form microstructures and textures of the‘Plattengneis’shear zone.Journal of Structural Geology,24(12):1957-1970.
Li W X and Li X H.2003.Adakitic granites within the NEJiangxi ophiolites,South China:Geochemical and Nd isotopic evidence.Precambrian Research,122(1):29-44.
Li Z X,Li X H,Jo A W,Chris C,Li X W,Zhang C L and Bao C M.2010.Magmatic and metamorphic events during the early Paleozoic Wuyi-Yunkai orogeny,southeastern South China:New age constraints and pressure temperature conditions.Geological Society of America Bulletin,122(5-6):772-793.
Lister G S and Dornsiepen U F.1982.Fabric transitions in the Saxony granulite terrain.Journal of Structural Geology,4(1):81-92.
Mainprice D,Bouchez J L,Blumenfeld P and Tubia J M.1986.Dominat c slip in naturally deformed quartz:Implication for dramatic plastic softening at high temperature.Geology,14:819-822.
Mercier J C,Anderson D A and Carter N L.1977.Stress in the lithosphere:Inferences from steady state flow of rocks.Pure and Applied Geophysics,115(1):199-226.
Parrish D K,Krivz A L and Carter N L.1976.Finite-element folds of similar geometry.Tectonophysics,32(3-4):183-207.
Passchier C W and Trouw R A.2005.Microtectonics.2nd Edition.Berlin:Springer:1-289.
Paterson M S and Luan F C.1990.Quartzite rheology under geological conditions.Geological Society,London,Special Publications,54(1):299-307.
Pfiffner O A and Ramsay J G.1982.Constraints on geological strainrates:Arguments from finite strain states of naturally deformed rocks.Journal of Geophysical Research,87(B1):311-321.
Poirier J P.1985.Creep of Cystals.New York:Cambridge University Press:1-260.
Prior D J and Wheeler J.1999.Feldspar fabrics in a greenschist facies albite-rich mylonite rom electron backscatter diffraction.Tectonophysics,303(1-4):29-49.
Stipp M,Stunitz H,Heilbronner R and Sechimid S M.2002.The eastern Tonale fault zone:“A natural laboratory”for crystal plastic deformation of quartz over a temperature range from 250 to 700℃.Journal of Structural Geology,24(12):1861-1884.
Stipp M and Tullis J.2003.The recrystallized grain size piezometer for quartz.Geophysical Research Letter,30(21):2008.
Stipp M,Tullis J,Scherwath M and Behmann J H.2010.Anew perspective on paleopiezometry:Dynamically recrystallized grain size distributions indicate mechanism changes.Geology,38(8):759-762.
Stünitz H,Gerald J D F and Tullis J.2003.Dislocation generation,slip systems,and dynamic recrystallization in experimentally deformed plagioclase single crystals.Tectonophysics,372(3):215-233.
Takahashi M,Nagahama H,Masuda T and Fujimura A.1998.Fractal analysis of experimentally,dynamically recrystallized quartz grains and its possible application as a strain rate meter.Journal of Structural Geology,20(2):269-275.
Toy V,Prior D J and Norris R J.2008.Quartz fabrics in the Alpine Fault mylonites:Influence of pre-existing preferred orientations on fabric development during progressive uplift.Journal of Structural Geology,30(5):602-621.
Twiss R J.1977.Theory and applicability of a recrystallized grain size paleopiezometer.Pure and Applied Geophysics,115(1):227-244.
Twiss R J.1980.Static theory of size variation with stress for subgrains and dynamically recrystallized grains//Magnitude of Deviatoric Stresses in the Earth’s Crust and Upper Mantle:Proceedings of Conference IX:Convened under Auspices of National Earthquake Hazards Reduction Program.Menlo Park,CA:US Geological Survey,80(625):665-683.
Wu R X,Zheng Y F,Wu Y B,Zhao Z F,Zhang S B,Liu X Mand Wu F Y.2006.Reworking of juvenile crust:Element and isotope evidence from Neoproterozoic granodiorite in South China.Precambrian Research,146(3):179-212.
Xu X B,Li Y,Tang S,Xue D and Zhang Z.2015.Neoproterozoic to Early Paleozoic polyorogenic deformation in the southeastern margin of the Yangtze Block:Constraints from structural analysis and 40Ar/39Ar geochronology.Journal of Asian Earth Sciences,98:141-151.
Xypolias P and Koukouvelas I K.2001.Kinematic vorticity and strain patterns associated with ductile extrusion in the Chelmos shear zone(External Hellenides,Greece).Tectonophysics,338(1):59-77.
Yao J L,Shu L S,Santosh M and Li J Y.2013.Geochronology and Hf isotope of detrital zircons from Precambrian sequences in the eastern Jiangnan Orogen:Constraining the assembly of Yangtze and Cathaysia Blocks in South China.Journal of Asian Earth Sciences,74(18):225-243.
Yu X Q,Wang D E,Jiang D Z,Jiang L L,Zhou X and Li CL.2011.Deformation stages and 40Ar/39Ar age data of the Wan-Zhe-Gan tectonic zone,southeast China,and their tectonic significance.Acta Geological Sinica(English Edition),85(6):1373-1389.
Zheng Y F,Wu R X,Wu Y B,Zhang S B,Yuan H L and Wu F Y.2008.Rift melting of juvenile arc-derived crust:Geochemical evidence from Neoproterozoic volcanic and granitic rocks in the Jiangnan Orogen,South China.Precambrian Research,163(3):351-383.
段留安,杨晓勇,孙卫东.2010.皖南天井山?小贺金矿区地质地球化学特征及找矿前景分析.矿床地质,29(S1):921-922.
段留安,杨晓勇,孙卫东,方世明,余良范,范增平.2011.皖南天井山金矿床地质?地球化学特征及找矿前景.地质学报,85(6):965-978.
高林志,丁孝忠,曹茜,张传恒.2010.中国晚前寒武纪年表和年代地层序列.中国地质,37(4):1014-1020.
高林志,杨明桂,丁孝忠,刘燕学,刘训,凌联海,张传恒.2008.华南双桥山群和河上镇群凝灰岩中的锆石SHRIMP U-Pb年龄--对江南新元古代造山带演化的制约.地质通报,27(10):1744-1751.
胡玲,刘俊来,纪沫,曹淑云,张宏远,张忠岩.2009.变形显微构造识别手册.北京:地质出版社:1-96.
黄学猛,张进江,许志琴.2016.电子背散射衍射(EBSD)技术在地壳构造变形研究中的应用.地质学报,90(6):1130-1145.
李建波,王涛,郭磊,童英,欧阳志侠,曾涛,史兴俊,张建军.2012.韧性剪切带的剪切作用类型和韧性减薄量.地质通报,31(1):26-37.
李婧,刘永江,李伟民,金巍,梁琛岳,温泉波,张媛媛.2016.华北克拉通基底花岗质片麻岩变形和流变学研究--以辽西寺儿堡地区为例.大地构造与成矿学,40(5):891-907.
李小兵,裴先治,陈有炘,刘成军,李佐臣,李瑞保,陈国超,魏博.2015.东昆仑造山带东段哈图沟-清水泉-沟里韧性剪切带塑性变形及动力学条件研究.大地构造与成矿学,39(2):208-230.
梁琛岳,刘永江,孟婧瑶,温泉波,李伟民,赵英利,米晓楠,张丽.2015.舒兰韧性剪切带应变分析及石英动态重结晶颗粒分形特征与流变参数估算.地球科学,40(1):116-129.
刘俊来,曹淑云,邹运鑫,宋志杰.2008.岩石电子背散射衍射(EBSD)组构分析及应用.地质通报,27(10):1638-1645.
覃有晃,林南孙,王爱国.1990.安徽省歙县?休宁地区金矿成矿地质条件及成矿预测研究报告.安徽省地质矿产局332地质队.
舒良树,于津海,贾东,王博,沈渭洲,张岳桥.2008.华南东段早古生代造山带研究.地质通报,27(10):1581-1593.
王德恩,韩守玉,杨荷金.2003.安徽省休宁县山斗金矿天井山矿段详查地质报告.安徽省地质矿产局332地质队.
王积善,张均.2016.皖南天井山地区金矿与韧性剪切带的关系.矿业工程研究,31(2):65-69.
王积善,张均,王健.2016.皖南天井山地区大型韧性剪切带特征及EBSD石英组构分析.矿物岩石,36(1):96-105.
王强,赵振华,简平,许继峰,包志伟,马金龙.2004.德兴花岗闪长斑岩SHRIMP锆石U-Pb年代学和Nd-Sr同位素地球化学.岩石学报,20(2):315-324.
王新社,郑亚东,杨崇辉,侯贵廷.2001.用动态重结晶石英颗粒的分形确定变形温度及应变速率.岩石矿物学杂志,20(1):36-41.
王勇,余达淦,管太阳,刘平辉,巫建华.2002.赣东北地区早白垩世火山岩的岩石学及岩石化学特征.岩石矿物学杂志,21(1):31-40.
汪明辉.2017.皖南地区金矿类型与成矿地质条件剖析.资源信息与工程,32(1):32-33.
吴建阳,张均.2010.从天井山金矿和金山金矿的成矿特征对比谈天井山金矿的找矿前景及突破方向.矿床地质,29(S1):1003-1004.
吴荣新,郑永飞,吴元保.2005a.皖南新元古代花岗闪长岩体锆石U-Pb定年以及元素和氧同位素地球化学研究.岩石学报,21(3):587-606.
吴荣新,郑永飞,吴元保.2005b.皖南石耳山新元古代花岗岩锆石U-Pb定年以及元素和氧同位素地球化学研究.高校地质学报,11(3):364-382.
吴荣新,郑永飞,吴元保.2007.皖南新元古代井潭组火山岩锆石U-Pb定年和同位素地球化学研究.高校地质学报,13(2):282-296.
夏浩然,刘俊来.2011.石英结晶学优选与应用.地质通报,30(1):58-60.
向必伟,朱光,王勇生,谢成龙,胡召齐.2007.糜棱岩化过程中矿物变形温度计.地球科学进展,22(2):126-134.
许志琴,王勤,梁凤华,陈方远,徐翠萍.2009.电子背散射衍射(EBSD)技术在大陆动力学研究中的应用.岩石学报,25(7):1721-1736.
徐海军,金淑燕,郑伯让.2007.岩石组构学研究的最新技术--电子背散射衍射(EBSD).现代地质,21(2):213-225.
徐先兵,汤帅,林寿发.2016.赣北景德镇韧性剪切带两类剪切指向及其构造意义.高校地质学报,22(2):308-316.
薛怀民,马芳,宋永勤,谢亚平.2010.江南造山带东段新元古代花岗岩组合的年代学和地球化学:对扬子与华夏地块拼合时间与过程的约束.岩石学报,26(11):3215-3244.
薛怀民,汪应庚,马芳,汪诚,王德恩,左延龙.2009.皖南太平?黄山复合岩体的SHRIMP年代学:由钙碱性向碱性转变对扬子克拉通东南部中生代岩石圈减薄时间的约束.中国科学(D辑),39(7):979-993.
杨昔林,曹殿华,李以科,黄玉凤,阚迎松,刘盛祥.2011.江西德兴孔家?银山火山盆地的时代归属:锆石U-Pb年代学证据.中国地质,38(1):86-108.
余心起,江来利,许卫,邱瑞龙,杜建国,戴圣潜.2007.皖浙赣断裂带的界定及其基本特征.地学前缘,14(3):102-13.
俞云文,徐步台,陈江峰,董传万.2001.浙东南中生代晚期火山岩Nd同位素组成及其地层学意义.高校地质学报,7(1):62-69.
张秉良,刘瑞珣,向宏发,楚全芝,黄雄南,郑勇刚.2008.红河断裂带中南段糜棱岩分形特征及主要流变参数的估算.地震地质,30(2):473-483.
张波,张进江,郭磊.2006.北喜马拉雅穹隆带然巴韧性剪切带石英动态重结晶颗粒的分维几何分析与主要流变参数的估算.地质科学,41(1):158-169.
张彦杰,周效华,廖圣兵,张晓东,武彬,王存智,余明刚.2010.皖赣鄣公山地区新元古代地壳组成及造山过程.地质学报,84(10):1401-1427.
赵崇贺,何科昭,邰道乾,乐昌硕,聂泽同.1997.赣东北地区重要火成岩的40Ar/39Ar年龄.地球科学,22(3):257-260.
郑蕾,周永章,曾长育.2013.钦杭结合带(南段)庞西垌断裂中动态重结晶石英颗粒分形特征及主要流变参数估算.中山大学学报(自然科学版),52(2):106-114.
周涛发,袁峰,侯明金,杜建国,范裕,朱光,岳书仓.2004.江南隆起带东段皖赣相邻区燕山期花岗岩类的成因及形成的地球动力学背景.矿物岩石,24(3):65-71.
周翔,余心起,王德恩,张德会,李春麟,傅建真,董会明.2011.皖南东源含W、Mo花岗闪长斑岩及成矿年代学研究.现代地质,25(2):201-210.
Bailey C M and Eyster E L.2003.General shear deformation in the Pinaleno Mountains metamorphic core complex,Arizona.Journal Structural Geology,25(11):1883-1893.
Boutonnet E,Leloup P H,Sassier C,Gardien V and Ricard Y.2013.Ductile strain rate measurements document long-term strain localization in the continental crust.Geology,41(8):819-822.
Charvet J,Shu L S,Shi Y S,Guo L Z and Faure M.1996.The building of south China:Collision of Yangzi and Cathaysia blocks,problems and tentative answers.Journal of Asian Sciences,13(3-5):223-235.
Chu Y and Lin W.2014.Phanerozoic polyorogenic deformation in southern Jiuling massif,northern South China block:Constraints from structural analysis and geochronology.Journal of Asian Sciences,86(3):117-130.
Faure M,Shu L,Wang B,Charvet J,Choulet F and MoniéP.2009.Intracontinental subduction:A possible mechanism for the Early Palaeozoic Orogen of SE China.Terra Nova,21(5):360-368.
Hacker B R,Yin A,Christie J M and Snoke A W.1990.Differential stress,strain rate,and temperatures of mylonitization in the Ruby Mountains,Nevada:Implications for the rate and duration of uplift.Journal of Geophysical Research,95(B6):8569-8580.
Hirth G,Teyssier C and Dunlap W J.2001.An evaluation of quartzite flow laws based on comparisons between experimentally and naturally deformed rocks.International Journal of Earth Sciences,90(1):77-87.
Hirth G and Tullis J.1992.Dislocation creep regimes in quartz aggregates.Journal of Structural Geology,14(2):145-159.
Hirth G and Tullis J.1994.The brittle-plastic transition in experimentally deformed quartz aggregates.Journal of Geophysical Research Solid Earth,99(B6):11731-11747.
Jessup M J,Cottle J M,Newell D L,Searle M P,Law R Dand Tracy R J.2006.Vorticity of flow and dis-placement along the South Tibetan Detachment System,Gondasampa region,Tibet.Journal of Asian Earth Sciences,26:143.
Ji S C,Jiang Z T,Rybacki E,Wirth R,Prior D and Xia B,2004.Strain softening and microstructural evolution of anorthite aggregates and quartz-anorthite layered composites deformed in torsion.Earth and Planetary Science Letters,222(2):377-390.
Ji S C and Mainprice D.1987.Experimental deformation of sintered above and below the order-disorder transition.Geodinamica Acta,1(2):113-124.
Ji S C and Mainprice D.1988.Natural deformation fabrics of plagioclase:Implications for slip systems and seismic anisotropy.Tectonophysics,147(1):145-163.
Ji S C and Mainprice D.1990.Recrystallization and fabric development in plagioclase.Journal of Geology,98(1):65-79.
Ji S C,Rybacki E,Wirth R,Jiang Z T and Xia B.2005.Mechanical and microstructural characterization of calcium aluminosilicate(CAS)and Si O2/CAS composites deformed at high temperature and high pressure.Journal of the European Ceramic Society,25(4):301-311.
Koch P S.1983.Rheology and microstructures of experimentally deformed quartz aggregates.Los Angeles:Ph D Dissertation,University of California:1-464.
Koch P S,Christie J M,Ord A and George R P.1989.Effect of water on the rheology of experimentally deformed quartzite.Journal of Geophysical Research Solid Earth,94(B10):13975-13996.
Kruhl J H and Nega M.1996.The fractal shape of sutured quartz grain boundaries:Application as a geothermometer.Geologische Rundschau,85(1):38-43.
Kruhl J H,Nega M and Milla H E.1995.The Fractal Shape of Grain Boundary Sutures:Reality,Model and Application as a Geothermometer//Book of Abstracts,2nd International Conference on Fractal and Dynamic Systems in Geosciences,84:31-32.
Kurz W,Fritz H,Tenczer V and Unzog W.2002.Tectonometamorphic evolution of the Koralm Complex(Eastern Alps):Constrains form microstructures and textures of the‘Plattengneis’shear zone.Journal of Structural Geology,24(12):1957-1970.
Li W X and Li X H.2003.Adakitic granites within the NEJiangxi ophiolites,South China:Geochemical and Nd isotopic evidence.Precambrian Research,122(1):29-44.
Li Z X,Li X H,Jo A W,Chris C,Li X W,Zhang C L and Bao C M.2010.Magmatic and metamorphic events during the early Paleozoic Wuyi-Yunkai orogeny,southeastern South China:New age constraints and pressure temperature conditions.Geological Society of America Bulletin,122(5-6):772-793.
Lister G S and Dornsiepen U F.1982.Fabric transitions in the Saxony granulite terrain.Journal of Structural Geology,4(1):81-92.
Mainprice D,Bouchez J L,Blumenfeld P and Tubia J M.1986.Dominat c slip in naturally deformed quartz:Implication for dramatic plastic softening at high temperature.Geology,14:819-822.
Mercier J C,Anderson D A and Carter N L.1977.Stress in the lithosphere:Inferences from steady state flow of rocks.Pure and Applied Geophysics,115(1):199-226.
Parrish D K,Krivz A L and Carter N L.1976.Finite-element folds of similar geometry.Tectonophysics,32(3-4):183-207.
Passchier C W and Trouw R A.2005.Microtectonics.2nd Edition.Berlin:Springer:1-289.
Paterson M S and Luan F C.1990.Quartzite rheology under geological conditions.Geological Society,London,Special Publications,54(1):299-307.
Pfiffner O A and Ramsay J G.1982.Constraints on geological strainrates:Arguments from finite strain states of naturally deformed rocks.Journal of Geophysical Research,87(B1):311-321.
Poirier J P.1985.Creep of Cystals.New York:Cambridge University Press:1-260.
Prior D J and Wheeler J.1999.Feldspar fabrics in a greenschist facies albite-rich mylonite rom electron backscatter diffraction.Tectonophysics,303(1-4):29-49.
Stipp M,Stunitz H,Heilbronner R and Sechimid S M.2002.The eastern Tonale fault zone:“A natural laboratory”for crystal plastic deformation of quartz over a temperature range from 250 to 700℃.Journal of Structural Geology,24(12):1861-1884.
Stipp M and Tullis J.2003.The recrystallized grain size piezometer for quartz.Geophysical Research Letter,30(21):2008.
Stipp M,Tullis J,Scherwath M and Behmann J H.2010.Anew perspective on paleopiezometry:Dynamically recrystallized grain size distributions indicate mechanism changes.Geology,38(8):759-762.
Stünitz H,Gerald J D F and Tullis J.2003.Dislocation generation,slip systems,and dynamic recrystallization in experimentally deformed plagioclase single crystals.Tectonophysics,372(3):215-233.
Takahashi M,Nagahama H,Masuda T and Fujimura A.1998.Fractal analysis of experimentally,dynamically recrystallized quartz grains and its possible application as a strain rate meter.Journal of Structural Geology,20(2):269-275.
Toy V,Prior D J and Norris R J.2008.Quartz fabrics in the Alpine Fault mylonites:Influence of pre-existing preferred orientations on fabric development during progressive uplift.Journal of Structural Geology,30(5):602-621.
Twiss R J.1977.Theory and applicability of a recrystallized grain size paleopiezometer.Pure and Applied Geophysics,115(1):227-244.
Twiss R J.1980.Static theory of size variation with stress for subgrains and dynamically recrystallized grains//Magnitude of Deviatoric Stresses in the Earth’s Crust and Upper Mantle:Proceedings of Conference IX:Convened under Auspices of National Earthquake Hazards Reduction Program.Menlo Park,CA:US Geological Survey,80(625):665-683.
Wu R X,Zheng Y F,Wu Y B,Zhao Z F,Zhang S B,Liu X Mand Wu F Y.2006.Reworking of juvenile crust:Element and isotope evidence from Neoproterozoic granodiorite in South China.Precambrian Research,146(3):179-212.
Xu X B,Li Y,Tang S,Xue D and Zhang Z.2015.Neoproterozoic to Early Paleozoic polyorogenic deformation in the southeastern margin of the Yangtze Block:Constraints from structural analysis and 40Ar/39Ar geochronology.Journal of Asian Earth Sciences,98:141-151.
Xypolias P and Koukouvelas I K.2001.Kinematic vorticity and strain patterns associated with ductile extrusion in the Chelmos shear zone(External Hellenides,Greece).Tectonophysics,338(1):59-77.
Yao J L,Shu L S,Santosh M and Li J Y.2013.Geochronology and Hf isotope of detrital zircons from Precambrian sequences in the eastern Jiangnan Orogen:Constraining the assembly of Yangtze and Cathaysia Blocks in South China.Journal of Asian Earth Sciences,74(18):225-243.
Yu X Q,Wang D E,Jiang D Z,Jiang L L,Zhou X and Li CL.2011.Deformation stages and 40Ar/39Ar age data of the Wan-Zhe-Gan tectonic zone,southeast China,and their tectonic significance.Acta Geological Sinica(English Edition),85(6):1373-1389.
Zheng Y F,Wu R X,Wu Y B,Zhang S B,Yuan H L and Wu F Y.2008.Rift melting of juvenile arc-derived crust:Geochemical evidence from Neoproterozoic volcanic and granitic rocks in the Jiangnan Orogen,South China.Precambrian Research,163(3):351-383.
© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号 地址：北京市海淀区学院路29号 邮编：100083 电话：办公室：(+86 10)66554848；文献借阅、咨询服务、科技查新：66554700 |