地球科学进展 ›› 2000, Vol. 15 ›› Issue (4): 467 -469. doi: 10.11867/j.issn.1001-8166.2000.04.0467

新科学新技术新方法 上一篇    下一篇

构造形成时限测定方法的探索
刘德良,曹高社,杨晓勇,方国庆   
  1. 中国科技大学地球与空间科学系;第三世界科学院地球和天文学高级研究中心,安徽 合肥 230026
  • 收稿日期:1999-11-23 修回日期:2000-03-17 出版日期:2000-08-01
  • 通讯作者: 刘德良(1938-),男,安徽凤阳人,教授,主要从事构造地球化学、构造岩石学、地质年代学等教学和研究工作。

EXPLORATION OF THE TIMING METHODS OF TECTONIC PROCESS

LIU De-liang, CAO Gao-she, YANG Xiao-yong,FANG Guo-qing   

  1. Department of Earth and Space Sciences,University of Science and Technology of China;Earth Science and Astronomy Senior Research Center,Science Institute of the Third World,Hefei230026,China
  • Received:1999-11-23 Revised:2000-03-17 Online:2000-08-01 Published:2000-08-01

地质作用过程持续时间的确定具有重要意义。前人已建立的地质定年方法(同位素法、古生物法和古地磁法)给出的是地质事件的“绝对年龄”或相对年代。但至今国内外尚缺乏有关地质作用持续时间的直接的测定方法。讨论了从构造地质学角度直接测定地质事件时限的一种新方法。

Geological timing methods established(isotopic method, paleontologic method,paleomagnetic method)set the“absolute age”or relative era of certain time in the geological process.But there have been no direct methods to measure the time limits of geological processes whether abroad or domestically so far. The tectonic chemical timing method we discussed, here is a new method which fixed the approxi-mate quantification of time limits in the tectonic geological processes.

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[1] 简平,杨巍然. 造山带构造年代学基本问题——论同位素体系与变质作用的关系[J]. 地球科学进展, 1998, 13(5): 452-457.
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