新生代东亚地形、水系与生物地理演变&#x02014;&#x02014;第三届地球系统科学大会拾翠

郑洪波; 郭正堂; 邓涛

doi:10.11867/j.issn.1001-8166.2014.11.1280

地球科学进展 >

2014 , Vol. 29 >Issue 11: 1280 - 1286

DOI: https://doi.org/10.11867/j.issn.1001-8166.2014.11.1280

新生代东亚地形、水系与生物地理演变——第三届地球系统科学大会拾翠

郑洪波 ,
郭正堂 ,
邓涛

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1. 南京师范大学地理科学学院, 南京, 210023
2. 中国科学院地质与地球物理研究所, 北京, 100029
3. 中国科学院古脊椎动物与古人类研究所, 北京, 100044

作者简介：郑洪波(1965-), 男, 山东乳山人, 教授, 主要从事构造—地貌与新生代环境演化研究. E-mail: zhenghb@njnu.edu.cn

网络出版日期: 2014-11-20

基金资助

中国科学院战略性先导科技专项项目“青藏高原多圈层相互作用及其资源环境效应”(编号：XDB03020301)资助．

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, 2014,

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Evolution of Topography, Drainage and Biogeography in East Asia during the Cenozoic: Summary of the Third Conference on Earth System Science

Hongbo Zheng ,
Zhengtang Guo ,
Tao Deng

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1. School of Geopgaphy Science, Nanjing Normal University, Nanjing, 210023
2. Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, 100029
3. Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, Beijing 100044

Online published: 2014-11-20

Copyright

地球科学进展编辑部, 2014, This is an open-access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.

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摘要

新生代期间, 亚洲及周边地区地球深部过程与地表环境发生了一系列重大变革。印度板块—欧亚板块碰撞和太平洋板块俯冲驱动下的构造—地貌过程, 导致青藏高原隆升、亚洲东部岩石圈伸展减薄、西太平洋边缘海扩张, 并最终塑造了现今的宏观地形地貌和水系格局。这一系列构造地貌过程与新生代全球气候变冷、西风环流与亚洲季风环流重组、生物地理演变之间存在紧密的关联, 成为地球科学领域重大前沿与热点课题, 是开展地球深部与浅表过程、地球表层各圈层之间相互作用研究的重要切入点。

关键词： 新生代; 亚洲; 构造—地貌; 生物地理

本文引用格式

郑洪波 , 郭正堂 , 邓涛 . 新生代东亚地形、水系与生物地理演变——第三届地球系统科学大会拾翠[J]. 地球科学进展, 2014 , 29(11) : 1280 -1286 . DOI: 10.11867/j.issn.1001-8166.2014.11.1280

Abstract

Drastic changes in the deep Earth processes and paleoenvironments on the surface occurred in Asia and surrounding regions during the Cenozoic. Driven by India-Asia collision and Pacific plate subduction, the Tibet Plateau region in the west gained its high elevation, whereas lithosphere in east China lost its thickness, and West Pacific margin seas opened, all of which led to the establishment of the present-day topography and drainage pattern. These tectonic-geomorphic processes interplayed with global cooling, re-organization of northern westerlies, Asian monsoon regime and biogeography in this region, which have become the frontier topics in earth sciences.

Key words： Cenozoic; Asia; Tectonicgeomorphology; Biogeography.

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