造山带概念的由来与演变及问题探讨  

Origin and evolution of the concept "Orogen"

作　　者：王东[1] 宋海峰[2] 单玄龙[2] 

机构地区：[1]贵州省113地质队,贵州六盘水553000 [2]吉林大学地球科学学院

出　　处：《吉林地质》2008年第3期52-55,共4页Jilin Geology

摘　　要：造山运动和造山带是被广泛应用和影响较大的两个古老概念,一百多年来随着地球科学的快速发展和板块构造理论的问世,情况已发生很大的变化。如何修订这一概念的内涵使之适应新的认识而又保持原定义的首尾一贯性正受到普遍关注。本文回顾了上述概念产生的历史背景,分析了它们在板块构造理论框架下、特别是在现今大陆构造研究中所面临的问题,本文认为对这一古老概念应进行重新修订、增补或再定义。The terms "orogeny" and "orogen" are both ancient classical concepts,which are widely used and have extensive influence.Following the rapid development of geosciences and the introduction of the plate tectonic theory during the past a hundred and more years,the situation has greatly change.How to refine these concepts so that they can be adaptive to modern understanding and meanwhile retain their original definitions have drawn wide attention.This paper presents a review of the historical background in whic...

关 键 词：造山带概念 造山作用 大陆构造 

分 类 号：P542.1[天文地球—构造地质学]