收稿日期: 2007-01-01
修回日期: 2007-01-01
网络出版日期: 2007-02-10
基金资助
国家自然科学基金项目“晓天—磨子潭断裂的演化对大别造山带折返的指示”（编号：40602025）资助.
Mineral Deformation Thermometer for Mylonitization
Received date: 2007-01-01
Revised date: 2007-01-01
Online published: 2007-02-10
向必伟 , 王勇生 , 胡召齐 , 谢成龙 , 朱光 . 糜棱岩化过程中矿物变形温度计[J]. 地球科学进展, 2007 , 22(2) : 126 -135 . DOI: 10.11867/j.issn.1001-8166.2007.02.0126
There has been no ideal means to constrain deformation temperatures of mylonites developed under low-moderate temperature conditions. However, it is necessary to determine the deformation temperature in studies of ductile shear zones. Based on new research achievements about the deformation of minerals, such as feldspar, quartz and calcite, this paper summaries approaches for estimating deformations temperatures by mineral deformation phenomena. Under different temperature conditions, deformations of feldspar and quartz show different stages, and their deformation and types of dynamic recrystallisation are closely related to temperatures. Slip systems and C-axis patterns of quartz as well as calcite e twin also exhibit differences with increasing temperatures. Microstructures of the minerals in mylonites can be used as thermometers to determine deformation temperatures.
Key words： Temperature estimate; Deformation; Dynamic recrystallisation.
[1]Walshe J L. A six-component chlorite solid solution model and the systems[J]. Economical Geology,1986, 81: 681-703.
[2]Essene E J. The current status of thermobarometry in metamorphic rocks[J].American Mineralogist,1989, 74: 1-44.
[3]Hoish T D. A muscovite-biotite geothermometer[J]. American Mineralogist,1989, 74: 565-572.
[4]Mancktelow N S, Pennacchioni G. The influence of grain boundary fluids on the microstructure of quartz-feldspar mylonites[J]. Journal of Structural Geology, 2004, 26: 47-69.
[5]Passchier C W, Trouw R A J. Micro-tectonics[M]. Springer-verlag Berlin Heidelberg,1996:36-45.
[6]Stipp M, Stünitz H, Heilbronner R, et al. The eastern Tonale fault zone: A natural laboratory' for crystal plastic deformation of quartz over a temperature range from 250 to 700℃[J]. Journal of Structural Geology,2002, 24:1 861-1 884.
[7]Sibson R H. Fault rock distribution and structure within the Alpine fault zone: A preliminary account[J]. Bulletin of the Royal Society of New Zealand,1999, 18:55-66.
[8]Van D. Orientation analysis of localized shear deformation in quartz fibres at the brittle-ductile transition[J]. Tectonophysics,1999, 303: 83-107.
[9]Hirth G, Tullis J. Dislocation creep regimes in quartz aggregates[J]. Journal of Structural Geology,1992,14:145-159.
[10]Neil S Mancktelow. The influence of grain boundary fluids on the microstructure of Quartz-feldspar Mylonites[J]. Journal of Structural Geology,2004,26: 47-69.
[11]White S H. Geological significance of recovery and recrystallization processes in quartz[J]. Tectonophysics,1977, 39: 143-170.
[12]Drury M R,Urai J L. Deformation-related recrystallization processes[J]. Tectonophysics,1990, 172:235-253.
[13]Schofield D L, Dlemos R S. Relationship between syn-tectonic granite fabric and regional P-T-t-d paths: An example from the Gander-Aralon boundary of NE Newfounelland[J]. Journal of Structural Geology,1998, 30:459-471.
[14]Lister G S, Dornsiepen U F. Fabric transitions in the Saxony granulite terrain[J]. Journal of Structural Geology,1982, 41: 81-92.
[15]Law R D. Crystallographic fabrics: A selective review of their applications to research in structural geology[C]//Knipe R J, Rutter E H, eds. Deformation Mechanisms, Rheology and Tectonics. Geological Society Special Publication, 1990, 54: 335-352.
[16]Bouchez J L. Plastic deformation of quartzites at low temperatures in an area of natural strain gradient[J]. Tectonophysics, 1997, 39: 25-50.
[17]Mainprice D, Bouchez J L, Blumendeld P. Domiant c-slip in naturally deformed quartz: Implications for dramatic plastic softening at high temperature[J]. Geology, 1986, 14: 819-822.
[18]Tullis J, Yund R A. Transition from cataclastic flow to dislocation creep of feldspar: Mechanisms and microstructures[J]. Geology, 1987, 15:606-609.
[19]Pryer L L. Microstructures in feldspars from a major crustal thrust zone: The Grenville Front, Ontario, Canada[J]. Journal of Structural Geology, 1993, 15: 21-36.
[20]Borges F S, White S H. Microstructural and chemical studies of sheared anorthosites, Roneval, South Harris[J]. Journal of Structural Geology, 1980, 2: 237-280.
[21]Gapais D. Shear structures within deformed granites: Mechanical and thermal indications[J]. Geology, 1989, 17:1 144-1 147.
[22]Gates A E, Glover L. Alleghanian tectono-thermal evolution of the dextral transcurrent hylas zone, Virginia Piedmont, USA[J]. Journal of Structural Geology, 1989, 11:407-419.
[23]Tullis J, Yund R A. Diffusion creep in feldspar aggregates: Experimental evidence[J]. Journal of Structural Geology, 1991, 13: 987-1 000.
[24]Vidal J L, Debat P, Soula J C. Ddformation and dynamic recrystallization of K-feldspar augen in orthogneiss from montagne Noire, Occitania, Southern France[J]. Lithos,1980, 13: 247-255.
[25]Olsen T S, Kohlstedt D L. Natural deformation and recrystallization of some intermediate plagioclase feldspars[J]. Tectonophysics, 1985, 111: 107-131.
[26]Hay R S, Evans B. Chemically induced grain boundary migration in calcite: Temperature dependence, phenomenology, and possible applications to geologic systems[J]. Contributions to Mineralogy and Petrology, 1987, 97: 77-87.
[27]Rosenberg C L. Deformation and recrystallization of plagioclase along a temperature Gradient: An example from the Bergell tonalite[J]. Journal of Structural Geology, 2003, 25: 389-408.
[28]Yund R A, Tullis J. Compositional changes of minerals associated with dynamic recrystallization[J]. Contributions to Mineralogy and Petrology, 1991, 97: 346-355.
[29]Lafrance B, John Barbara E, Frost B R. Ultra high-temperature and subsolidus shear zones: Examples from the Poe Mountain anorthosite, Wyoming[J]. Journal of Structural Geology, 1998, 20: 945-955.
[30]Anderson D J, Lindsley D H, Dabidson P M. QUILF: A Pascal program to assess equilibria among Fe-Mg-Mn-Ti oxides, pyroxenes, olivine, and quartz[J]. Computers and Geosciences,1993, 19: 1 333-1 350.
[31]Altenberger U. Ductile deformation of K-feldspar in dry eclogite facies shear zones in the Bergen Arcs, Norway[J]. Tectonophysics, 2000, 320: 107-121.
[32]Ferrill D A, Morris A P, Evans M A,et al. Calcite twin morphology: A low-temperature deformation geothermometer[J]. Journal of Structural Geology, 2004,26:1 521-1 529.
[33]Zhu Guang, Xie Chenglong, Wang Yongsheng, et al. Characteristics of the Tan-Lu high-Pressure strike-slip ductile shear zone and its 40Ar/39Ar dating[J]. Acta Petrologica Sinica, 2005, 21(6): 1 687-1 702.
[34]Wang Yongsheng, Zhu Guang, Chen Wen, et al. Thermochronologic information from the Tan-Lu fault zone and its relationship with the exhumation of the Dabie Mountains[J]. Geochimica, 2005, 34(3): 193-214. [王勇生, 朱光, 陈文,等. 郯庐断裂带热年代学信息及其与大别造山带折返的关系[J]. 地球化学, 2005, 34(3): 193-214.]
[35]McDougall I, Harrison T M. Geochronology and Thermochonology by the 40Ar /39Ar Method[M]. New York: Oxford University Press, 1998.
[36]Dodson M H. Closure temperature in cooling geochronological and petrological systems[J]. Contributions to Mineralogy and Petrology, 1973, 40(30): 259-174.
[37]Harrison T M. Diffusion of 40Ar in hornblende[J]. Contributions to Mineralogy and Petrology, 1981, 78: 324-331.
[38]Reddy S M, Kelley S P, Magennis L. A microstructural and argon laserprobe study of shear zone development at the western margin of the Nanga Parbat-Haramosh Massif, western Himalaya[J]. Contributions to Mineralogy and Petrology, 1997, 128: 16-29.
[39]Zhu Guang, Niu Manlan, Liu Guosheng, et al. 40Ar/39Ar Dating for the strike-slip movement on the Feidong Part of the Tan-Lu Fault belt[J]. Acta Geologica Sinica,2005, 79(3):303-316. [朱光, 牛漫兰, 刘国生,等.郯庐断裂带肥东段走滑运动的40Ar/39Ar 法定年[J]. 地质学报, 2005, 79(3):303-316.]
[40]Zhu Guang, Wang Yongsheng, Liu Guosheng, et al. 40Ar/39Ar dating of strike-slip motion on the Tan-Lu fault zone，East China[J]. Journal of Structural Geology, 2005, 27（8）:1 379-1 398.
[41]Zhu Guang, Wang Daoxuan, Liu Guosheng,et al. Extensional activities along the Tan-Lu fault zone and its geodynamic setting[J]. Scientia Geologica Sinica,2001, 36(3):269-278. [朱光, 王道轩, 刘国生,等. 郯庐断裂带的伸展活动及其动力学背景[J]. 地质科学, 2001, 36(3):269-278.]
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