地球科学进展 ›› 1998, Vol. 13 ›› Issue (2): 157 -160. doi: 10.11867/j.issn.1001-8166.1998.02.0157

干旱气候变化与可持续发展 上一篇    下一篇

岩石古流变性质的构造研究进展
曾佐勋,付永涛   
  1. 中国地质大学地学院 武汉 430074
  • 收稿日期:1997-05-26 修回日期:1997-10-13 出版日期:1998-04-01
  • 通讯作者: 曾佐勋
  • 基金资助:

    国家教委博士点基金资助项目“高波幅褶皱主波长理论的物理实验与地质观测研究”( 项目编号: 9349103) 资助.

ADVANCES IN STRUCTURAL STUDY OF PALEO-RHEOLOGICAL PROPERTIES OF ROCKS

Zeng Zuoxun,Fu Yongtao   

  1. Faculty of Earth Sciences, China University of Geosciences, Wuhan  430074
  • Received:1997-05-26 Revised:1997-10-13 Online:1998-04-01 Published:1998-04-01

岩石古流变性质研究是大陆动力学研究的一个重要方面。岩石古流变性质研究的一个发展方向是通过比例模型,建立流变参数与构造变形几何参数之间的定量关系,再利用天然岩石构造变形几何参数的定量测定,反推在形成这些变形时所处物理化学条件下的岩石流变参数。对利用露头尺度地质构造的定量测量研究岩石古流变性质的方法与进展做了重点介绍。

The study of paleo-rheological properties of rocks is one of important aspects of continental dynamical research. One way of quantitative research on paleo-rheology of rocks is to estimate rock rheological parameters in the just physical-chemical environment in which rocks deformed, through measurement of geometric parameters of natural structural deformation of rocks in the quantitative connection, which is established by scale-model, of rock rheological parameters and geometric parameters of natural structural deformation. This paper introduces the advances of study on quantitative research on natural deformed rocks in methods of structural measurement.

中图分类号: 

[1] Heard H C,Raleigh C B. Steady-state flow in marble from 500℃ to 800℃. Geol Soc Am Bull, 1972, 83: 935~956.
[2] Rutter E H. The influence of temperature, strain rate and interstitial water in the experimental deformation of calcite rocks. Tectonophysics, 1974, 22:311~334.
[3] Nicolas A, Poirier J P. 变质岩的晶质塑性和固态流变. 林传勇, 史兰斌译. 北京: 科学出版社, 1985. 434~447.
[4] Turcotte D L, Schubert G. 地球动力学. 韩贝传等译. 北京:地震出版社, 1986. 284~337.
[5] Carter N L, Tsenn M C. Flow properties of continental lithosphere. Tectonophysics, 1987, 136:27~63.
[6] Jin Z M, Green H W, Zhou Y. Melttopology in partially molten mantle peridotite during ductile deformation. Nature, 1994, 372: 164~167.
[7] 金振民, 金淑燕, Green H W. 台湾海峡上地幔流变学状态及其构造意义. 地质学报, 1995, 69(1): 31~41.
[8] Ramsay J G. 岩石韧性及其对山带中构造发育的影响. 李智陵译. 基础地质译丛, 1985, 2:49~60,91.
[9] Ramsay J G, Huber M I. 现代构造地质学方法(第二卷). 褶皱和断裂. 徐树桐主译. 北京: 地质出版社, 1991. 78~143.
[10] 游振东, 索书田, 韩郁菁, 等. 造山带核部杂岩变质过程与构造解析. 武汉:中国地质大学出版社,1991.14~41.
[11] 傅昭仁, 单文琅, 成勇, 等. 北京西山的构造变形相分析. 见: 张吉顺, 单文琅. 北京西山地质研究. 武汉: 中国地质大学出版社, 1990.8~17.
[12] Kanagawa K. Competence contrasts in ductile deformation as illustrated from naturally deformed chert mudstone layers. J Struct Geol, 1993, 15(7): 865~885.
[13] Hudleston P J, Lan L. Information from fold shapes. J struct Geol, 1993, 15: 253~264.
[14] Hudleston P J, Lan L. Rheological controls on the shapes of single-layer folds. J Struct Geol, 1994, 16(7): 1 007~1 021.
[15] Lan L, Hudleston P J. Rock rheology and sharpness of folds in single layers. J Struct Geol, 1996, 18(7): 925~931.
[16] Masuda T, Shibutani T, Igayashi T, et al. Microboundin structure of piedomontite in quartz schists: a proposal for a new indicator of relative palaeodifferential stress. Tectonophysics, 1989, 163: 169~180.
[17] Masuda T, Shibutani T, Yamaguchi H. Practial stress analysis using piedomontite microboundinage structures. J struct Geol, 1995, 17(12): 1 793~1 795.
[18] Masuda T, Mizuno N, Kobayashi M, et al. 旋转剪切带中牛顿材料和非牛顿材料的应力和应变估测. 付永涛译. 地质科学译丛, 1997, 1: 14~16.
[19] 曾佐勋, 付永涛. 岩石流变性质的构造研究. 华南地质与矿产, 1996, (4) : 32~36.
[20] 曾佐勋, 付永涛, 李艳霞. 北京西山膨缩石香肠流变性质构造研究初探. 地质力学学报,1997,3(1):45~49.
[21] 付永涛, 曾佐勋, 朱永军. 单层纵弯褶皱曲率指数与应力指数的关系探讨. 地质科技情报, 1997, 16(1): 108~112.
[22] 金振民. 高温高压岩石变形实验及其地球动力学意义. 地质科技情报, 1988, 7(3): 11~19.
[23] 索书田. 大陆岩石圈流变学研究. 地质科技情报, 1992, 11(2): 6~10.
[24] Treagus S H. Strain refraction in layered system. J Struct Geol, 1988, 10: 517~527.
[25] Smith R B. Unified theory of the onset of folding, boundinage, and million structures. Bull Geol Soc Am, 1975, 86: 1 601~1 609.
[26] Smith R B. Formation of folds, boundinages, and mullions in non-New tonian materials. Bull Geol Soc Am, 1977, 88:312~320.
[27] Emerman S E, Turcotte D L. A back-of-the envelop approach to boundinage mechanics.Tectonoph ysics,1984,110:333~338.
[28] 王仁. 大地构造分析中的一些力学问题. 力学进展, 1989, 19(2): 145~157.
[29] 曾佐勋, 刘立林. 构造模拟. 武汉: 中国地质大学出版社, 1992. 10.

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