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DOI | 10.1007/s11430-016-5014-6 |
Dynamics of unstable continental subduction: Insights from numerical modeling | |
Huangfu PengPeng; Wang YueJun; Fan WeiMing; Li ZhongHai; Zhou YongZhi | |
通讯作者 | Wang, YJ (通讯作者) |
发表日期 | 2017 |
ISSN | 1674-7313 |
EISSN | 1869-1897 |
起始页码 | 218 |
结束页码 | 234 |
卷号 | 60期号:2 |
英文摘要 | Numerical experiments are used in this study to systematically investigate the effects of convergence rate, crustal rheological strength, and lithospheric thermal structure on the dynamics of continental collision. The study focuses on the types, conditions and processes of unstable continental subduction. Modelling results suggest that the development of unstable continental subduction can be promoted by conditions that tend to decrease rheological strength of the lithosphere, such as low crustal rheological strength, hot thermal structure of the lithosphere, or low convergence rate. Unstable subduction mode can be further categorized into three types: (1) multi-stage slab breakoff, (2) continuously flowing of fluid-like slab into the upper mantle, and (3) large-scale detachment of the thickened orogenic root. These three types of unstable continental subduction are respectively associated with (1) a low convergence rate, (2) hot thermal structure of the lithosphere with a high convergence rate, and (3) moderate-high crustal rheological strength with a low convergence rate. It is also revealed that the evolution of crustal melting is dominated by the deformation pattern of continental collision, which is mainly controlled by crustal rheological strength. The modelling results have important implications for understanding of continental subduction mode selection under specific geodynamic conditions. |
关键词 | INDIAN LITHOSPHERE BENEATHCOLLISIONAL OROGENSTIBETAN PLATEAUCENTRAL-ASIAZONESROCKSEXHUMATIONRHEOLOGYINSTABILITIESMETAMORPHISM |
英文关键词 | Unstable continental subduction; Stable continental subduction; Slab breakoff; Detachment; Partial melting |
语种 | 英语 |
WOS研究方向 | Geology |
WOS类目 | Geosciences, Multidisciplinary |
WOS记录号 | WOS:000394043000002 |
来源期刊 | SCIENCE CHINA-EARTH SCIENCES
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来源机构 | 中国科学院青藏高原研究所 |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/258948 |
推荐引用方式 GB/T 7714 | Huangfu PengPeng,Wang YueJun,Fan WeiMing,et al. Dynamics of unstable continental subduction: Insights from numerical modeling[J]. 中国科学院青藏高原研究所,2017,60(2). |
APA | Huangfu PengPeng,Wang YueJun,Fan WeiMing,Li ZhongHai,&Zhou YongZhi.(2017).Dynamics of unstable continental subduction: Insights from numerical modeling.SCIENCE CHINA-EARTH SCIENCES,60(2). |
MLA | Huangfu PengPeng,et al."Dynamics of unstable continental subduction: Insights from numerical modeling".SCIENCE CHINA-EARTH SCIENCES 60.2(2017). |
条目包含的文件 | 条目无相关文件。 |
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