青藏滇缅印尼歹字型构造再认识

赵越; 闫纪元

doi:10.12090/j.issn.1006-6616.2019.25.05.067

青藏滇缅印尼歹字型构造再认识

赵越^1,2,,
闫纪元^1,2

1.
中国地质科学院地质力学研究所, 北京 100081

2.
自然资源部古地磁与古构造重建重点实验室, 北京 100081

基金项目:
中国地质科学院院长基金（JYYWF201819）；国家自然科学基金（41672062）

详细信息

作者简介: 赵越(1955-), 男, 研究员, 构造地质学专业, 主要从事大地构造及极地地质研究等。E-mail:yue_zhao@cags.ac.cn

中图分类号: P542

责任编辑:范二平

收稿日期: 2019-08-30

修回日期: 2019-10-12

刊出日期: 2019-10-31

REDISCOVERING OF THE QINGHAI-TIBET-YUNNAN-BURMA-INDONESIAN η-TYPE STRUCTURE

ZHAO Yue^1,2,,
YAN Jiyuan^1,2

1.
Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China

2.
Key Laboratory of Paleomagnetism and Tectonic Reconstruction, Ministry of Natural Resources, Beijing 100081, China

Received Date: 30 August 2019

Revised Date: 12 October 2019

Publish Date: 31 October 2019

摘要

摘要:
青藏滇缅印尼歹字型自中新世中期澳大利亚板块与东南亚大陆开始碰撞逐渐形成。上新世早期演化成为具有统一形变、运动和动力体系的构造。其与澳大利亚以及西南太平洋地区的连环式旋卷构造是一个构造整体，可以归入一个构造体系。探索认识这一巨型构造体系因其与青藏高原构造地貌的演变，全球大洋温盐环流的重大调整密切相关。其导致了区域乃至影响了全球的气候环境剧变。认识李四光教授的科学思想和构造体系需要沿着其思想脉络，从更广阔的范围和科学发展的前沿思考和探索。
- 青藏滇缅印尼歹字型 /
- 构造体系 /
- 中期中新世 /
- 早期上新世 /
- 东南亚 /
- 澳大利亚
Abstract:
The Qinghai-Tibet-Yunnan-Burma-Indonesian η-type structure was gradually shaped from Middle Miocene when the earliest collision between the Australia plate and the Southeast Asia blocks began. This tectonic system has been formed since Early Pliocene with a unified deformation, motion and dynamical system. It belongs to a huge tectonic system with the serial vortex structures extending from southeastern Asia to Australia and the southwestern Pacific. Rediscovering of this tectonic system is because of that it is closely related to the tectonic geomorphic evolution of Tibet Plateau and the significant adjustment of the global ocean thermohaline current which caused to regional and even global climate change. To understand Professor J.S.Lee's scientific thought and his tectonic system theory needs to think and explore from a broader scope and the frontier of scientific development along the essence of his thought.
- Qinghai-Tibet-Yunnan-Burma-Indonesian η-type structure /
- tectonic system /
- Middle Miocene /
- Early Pliocene /
- Southeast Asia /
- Australia

HTML全文

图 1 澳大利亚-巴布亚新几内亚陆块与南极大陆在渐新世初期分离^[7]

Figure 1.

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图 2 澳大利亚-巴布亚新几内亚陆块与东南亚大陆碰撞过程^[8]

Figure 2.

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图 3 喜马拉雅东构造结的形成^[9]

Figure 3.

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图 4 青藏高原及其周边地区相对于稳定欧亚板块的GPS速度场及东部分量随经纬度的变化

Figure 4.

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图 5 青藏滇缅印尼歹字型构造构造纲要图

Figure 5.

下载: 全尺寸图片幻灯片

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