地球科学进展 ›› 1994, Vol. 9 ›› Issue (2): 35 -40. doi: 10.11867/j.issn.1001-8166.1994.02.0035

干旱气候变化与可持续发展 上一篇    下一篇

造山带变质作用PTt轨迹研究存在的问题和发展趋势
庄育勋   
  1. 中国地质科学院地质研究所   北京   100037
  • 收稿日期:1993-02-17 出版日期:1994-03-01
  • 通讯作者: 庄育勋

SOME PROBLEMS EXSISTED IN RESEARCH OF OROGENIC METAMORPHIC PTt PATHS AND DEVELOPING TREND

Zhuang Yuxun   

  1.  Institute of Geology CAGS,Beijing  100037
  • Received:1993-02-17 Online:1994-03-01 Published:1994-03-01

目前的适山带变质作用PTt轨迹热模拟研究仍受变质作用程度由深度控制的传统观念的制约,其主要假定条件没有很好地反映造山带变质作用客观的和本质的特征,因而亦无法反映造山作用的真实过程和造山带变质作用的地质动因。造山带变质作用研究应朝着变质作用与构造变形作用、花岗岩化作用等多种地质作用综合研究、时间演化过程与三维空间变化特点有机结合、造山带变质作用时空演化特点与地幔深部地球动力学过程统一综合研究的方向发展。

    The present reseaching of forward modeling of orogenic metamorphism has been restrained by the thought that metamorphic grade is function of depth. Its assumption didn't reflected the insitric characteristics of orogenic metamorphism. The data from the reversing approaches indicates that the uneven gushing of thermal and structural flow in orogenic belt results in progressive metamorphism, granitization and progressive deformation and development of thermal-structural-gneiss dome.
    It is important developing trend to combine temporal evolution and three-dimentional spatial variation of progressive metamorphism, granitization and progressive deformation and construct a unified geodynamic system between orogenic metamorphism and the process of lithosphere movement under the orogenic belt.

 

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