地球科学进展 ›› 2002, Vol. 17 ›› Issue (4): 546 -550. doi: 10.11867/j.issn.1001-8166.2002.04.0546

综述与评述 上一篇    下一篇

花岗岩构造与侵位机制研究进展
杨坤光,刘强   
  1. 中国地质大学地球科学学院,湖北 武汉 430074
  • 收稿日期:2001-11-05 修回日期:2002-01-25 出版日期:2002-12-20
  • 通讯作者: 杨坤光(1954-),男,安徽滁州人,教授,主要从事构造地质学的教学和科研工作.E-mail:dxy07@cug.edu.cn E-mail:dxy07@cug.edu.cn
  • 基金资助:

    国家自然科学基金项目“大别山中生代花岗岩构造样式与变形序列研究”(编号:40172069)资助.

ADVANCES IN GRANITIC STRUCTURES AND EMPLACEMENT MECHANISMS

YANG Kun-guang,  LIU Qiang   

  1. Faculty of Earth Science, China University of Geosciences, Wuhan  430074, China
  • Received:2001-11-05 Revised:2002-01-25 Online:2002-12-20 Published:2002-08-01

近年来对造山带花岗岩构造与侵位机制的研究表明,花岗岩不但可以侵位在区域伸展的构造背景,也可以侵位在区域挤压(缩短)的构造背景。花岗岩侵位受断裂的控制并不是像以前认为的那样明显,而是受多种侵位机制的共同作用,而构造样式和变形组构则是侵位机制研究的基础。提出了一些新的研究思路和方法。此外,对大别山中生代花岗岩构造、侵位机制作了简要讨论。

 Great advances have been made on granitic structures and emplacement mechanisms in recent years. Studies on many granitoid plutons in different orogenic belts have got new conclusions: granitoid plutons not only emplaced in the regional extension setting, but also in the regional compressive (shortening) setting. The relationship between granitoid plutons and faults has been attentively investigated in orogenic belts recently. It is much unlikely thought before that emplaced granitoid pluton had been controlled by faults or fractures. In fact, the process of intruding and opening space must have been controlled by multiple emplacement mechanisms. Meanwhile, study on structural patterns and deformed fabrics of granitic pluton is the key to emplacement mechanisms. So we suggest some research ideas and  methods in this paper: studies on vertical structural pattern, use aluminium-in- hornblende  geobarometer  to determine an emplaced depth, tectonic analyses and deformation sequences, quantification studies on multiple emplacement mechanisms, etc. At last, we discuss the Mesozoic granitic structures and emplacement mechanisms in Dabie mountain orogen.  

中图分类号: 

[1]Wang Tao. Studies on granites and continental dynamics[J]. Earth Science Frontiers, 2000, 7(Suppl):137-146.[王涛. 花岗岩研究与大陆动力学[J]. 地学前缘,2000,7(增刊):137-146.]
[2]Evans N G, Gleizes  G, Leblans  D, et al. Syntectonic emplacement of the Maladeta granite (Pyrenees) deduced from relationships between Herecynian deformation contact metamorphism[J]. Journal of Geology  Society, 1998, 15:209-216.
[3]Yenes M, Alvarez F, Gutierrez-Alonso G. Granite emplacement in orogenic compressional conditions: the La Alberca-Bejar granitic area (Spanish Central System, VariscanIberian Belt) [J]. Journal of Structure  Geology, 1999,21:1 419-1 440.
[4]Davis B K, Henderson  R A. Syn-orogenic extensional and contractional deformation related to granite emplacement in the northern Tasman Orogenic zone, Australia[J]. Tectonoghysics,1999, 305:433-475.
[5]Pe-pier G, Koubouvelas I, Davis J  W.  Synkinematic granite emplacement in a shear zone: the Pleasant Hills pluton, Canadian Appalachians[J]. GSA Bulletin,1998, 110:523-536.
[6]McCaffrey K J L, Miller  C F,  Karlstrom  K E, et al. Synmagmatic deformation patterns in the Old Women Mountains, SE California[J]. J Struct Geol, 1999,21: 335-349.
[7]Paterson S R, Schmidt K L. Is there a close spatial relationship between faults and plutons[J]. J Struct  Geol, 1999,21:1 131-1 142.
[8]Pateroson  S R, Miller R B. Magma emplacement during arc-perpendicular shorting: an example from the cascades crystalline core, Washington[J]. Tectonics, 1988, 17(4): 571-586.
[9]Escuder  J V. Relationship between structural units in the Tormes gneise dome (NW Iberian massif, Spain): geometry structure and kinematics of contractional and extensional Variscan deformation[J]. Geol Rundsch, 1998,87:165-179.
[10]Hollister L S, Grissom G C. Confirmation of the empirical correlation of Al in hornblende with pressure of solidification of calc-alkaline plutons[J]. American Mineralogist, 1987,72(2): 231-239.
[11]Schmidt M W.  Amphibole composition in tonalite as a function of pressure barometer, Contrib[J]. Mineral  Petro,  1992,111:304-310.
[12]Yang Kunguang, Ma Changqian, Xu Changhai, et al.Differential uplift between Beihuaiyang and Dabie orogenic belt[J]. Science in China (D), 2000, 43(2): 193-199.[杨坤光,马昌前,许长海,等. 北淮阳构造带与大别造山带的差异性隆升[J].中国科学(D),2000,43(2):193-199.]
[13]Ai Xiaoling, Ma Changqian. Mineral chemistry of amphiboles and feldspars from liujiawa syn-exhumation intrusive in the Dabie orogen [J]. Atca Mineralogica Sinica, 2000, 20(3): 213-219.[艾晓玲,马昌前. 大别山同剥露刘家洼杂岩体角闪石、长石的矿物化学[J].矿物学报,2001,20(3):213-219.]
[14]Chofield D L, Dlemos R S.Relationship between syn-tectonic granite fabric and regional PTtd paths: an example from the Gander-Avalon boundary of NE Newfoundland[J].J Stouct Geology, 1998,30: 459-471.
[15]Shigematsu N, Tanaka H. Dislocation creep of fne-grained recrystallized plagioclase under low-tempreature condition[J]. J Struct Geology, 2000,32: 65-69.
[16]Wang Z H, Lu H F. Dectile deformation and Ar/Ar dating of the Changle-Nanao ductile shear zone, southeastern China[J]. J Struct Geology, 2000, 22: 561-570.
[17]Zheng Rongcai. Application of ESR dating to petroleum geology [J]. Oil and Gas Geology, 1998, 19(2): 93-98.[郑荣才,ERS测年在石油地质研究中的应用[J].石油与天然气地质,1998,19(2):93-98.]
[18]Hutton D H W, Reary R J. A new mechanism of granite emplacement: intrusion in active extensional shear zone[J]. Nature, 1990, 343: 452-455.
[19]Paterson S R, Rernon R H. Bursting the bubble of ballooning plutons: a return to nested diapers emplaced by multiple process[J]. Geol Soc America Bulletin, 1995, 107: 1 356-1 380.
[20]Castro A, Fernandez C. Granite intrusion by externally induced growth and deformation of magma reservoir, the example of the Plasenzuela pluton, Spain[J]. J Struct Geology, 1998, 20:1 219-1 228.
[21]Wang T, Wang X, Li W. Evaluation of multiple emplacement mechanisms: the Huichizi granite pluton, Qinling orogenic belt, central China[J]. J Strct Geol, 2000,22:505-518.
[22]Ma C, Li Z, Ehlers C, et al. A post-cdlisional magmatic plumbing system: Mesozoic granitoid plutons from the Dabieshan high-pressure and ultrahigh-Pressure metamorphic zone, east-central China[J]. Lithos,1988, 45: 431-456.
[23]Zhang Hongfei ,Zhong Zengqiu,Gao Shan, et al.Zircon U-Pb ages of the foliated garnet-bearing granites in the western Dabie Monutains[J]. China Science Bulletin, 2001,46(10):843-846.[张宏飞,钟增球,高山,等. 大别山西部面理化含榴花岗岩锆石U-Pb年龄[J].科学通报,2001,46(10):843-846.]

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