青藏高原隆生演化变形模式研究进展  

Summary and Current Status of the Research Models for the Tibetan Plateau Uplift

作　　者：马钦忠[1] 

机构地区：[1]上海市地震局,上海

出　　处：《自然科学》2016年第2期229-241,共13页Open Journal of Nature Science

基　　金：上海市科委科研计划项目(12231202700);国家自然科学基金项目(41090292);中国地震局星火项目(XH12016)资助。

摘　　要：多半个世纪以来国内外许多地球科学家对青藏高原的形成和演化进行多学科研究,各种构造变形模式的观点和假设相继出现,随着科学技术的发展和最新资料的不断积累,已有的一些模式不断被质疑、修正,新的模式不断出现。本文对11种模式进行追踪梳理、简洁综述,对一些模式的不足和质疑问题也予以简介,并对青藏高原构造演化变形模式研究现状进行了梳理,以期对全面认识青藏高原构造演化变形模式研究的过程有所裨益。For more than half a century, many geoscientists at home and abroad have carried out multi-dis- ciplinary research on the formation and evolution of the Tibetan Plateau. Various views and hy-pothesis of the tectonic formation models appeared successively. With the development of science and technology as well as the steady accumulation of the latest data, some existing models constantly are challenged and corrected, and new models unceasing put forward. In this paper the tracks of eleven models are followed and reviewed concisely, and the problem of the lack of some patterns and questions also are introduced briefly. The research status about the tectonic evolution and deformation models are also teased. It is hoped to benefit to comprehensively understanding the tectonic evolution and deformation models of the Tibetan Plateau.

关 键 词：青藏高原 印度板块 欧亚板块 隆升机制 

分 类 号：G6[文化科学—教育学]