Climate Change Data Portal
DOI | 10.1016/j.earscirev.2021.103622 |
Mantle micro-block beneath the Indian Ocean and its implications on the continental rift-drift-collision of the Tethyan evolution | |
Suo Y.; Li S.; Cao X.; Liu Y.; Zhu J.; Li X.; Somerville I. | |
发表日期 | 2021 |
ISSN | 0012-8395 |
卷号 | 217 |
英文摘要 | A series of ancient Tethys ocean basins have been consumed beneath the Indian Ocean and are hard to observe due to their subduction below the southern Eurasian margin. The presence of the delaminated Gondwana fragments beneath the Indian Ocean also has long been suspected. These microplate tectonics lead to a fairly complex shallow crust and deep mantle configuration, which makes it difficult to reconstruct East Gondwana and discuss the geodynamics of continental rift-drift-collision in the Tethyan Realm. Lithospheric or crustal thinning due to the dehydration of the underlying stagnant slab is a good tracer of the subducted plate. Using the gravity-derived oceanic crust and Euler rotation method, we obtained an asymmetric crustal thickness across the Indian Ocean ridges. Areas of anomalous intra-plate crustal thinning were revealed and applied to track the possible subducted slabs. Then, combined with other geophysical data, two Meso-Tethyan slabs, one Neo-Tethyan slab, and two Indian slabs were delimited. From north to south, the slabs beneath India and the Northeast Indian Ocean constitute a south-dipping and step-shaped architecture. It requires a double subduction zone or a two-stage India-Eurasia collision model to be driven by the slab pull, which is still open for debate. © 2021 Elsevier B.V. |
英文关键词 | Crustal thinning; Indian Ocean; Mantle micro-block; Subduction kinematics; Tethyan geodynamics |
语种 | 英语 |
scopus关键词 | continental collision; continental drift; crustal thinning; geodynamics; mantle; plate tectonics; subduction; tectonic evolution; tectonic reconstruction; Tethys; Indian Ocean; Tethys |
来源期刊 | EARTH-SCIENCE REVIEWS |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/209324 |
作者单位 | Frontiers Science Center for Deep Ocean Multispheres and Earth System, Key Lab of Submarine Geosciences and Prospecting Techniques, MOE and College of Marine Geosciences, Ocean University of China, Qingdao, 266100, China; Laboratory for Marine Mineral Resources, Qingdao National Laboratory for Marine Science and Technology, Qingdao, 266237, China; UCD School of Earth Sciences, University College Dublin, Belfield, Dublin 4, Ireland |
推荐引用方式 GB/T 7714 | Suo Y.,Li S.,Cao X.,et al. Mantle micro-block beneath the Indian Ocean and its implications on the continental rift-drift-collision of the Tethyan evolution[J],2021,217. |
APA | Suo Y..,Li S..,Cao X..,Liu Y..,Zhu J..,...&Somerville I..(2021).Mantle micro-block beneath the Indian Ocean and its implications on the continental rift-drift-collision of the Tethyan evolution.EARTH-SCIENCE REVIEWS,217. |
MLA | Suo Y.,et al."Mantle micro-block beneath the Indian Ocean and its implications on the continental rift-drift-collision of the Tethyan evolution".EARTH-SCIENCE REVIEWS 217(2021). |
条目包含的文件 | 条目无相关文件。 |
个性服务 |
推荐该条目 |
保存到收藏夹 |
导出为Endnote文件 |
谷歌学术 |
谷歌学术中相似的文章 |
[Suo Y.]的文章 |
[Li S.]的文章 |
[Cao X.]的文章 |
百度学术 |
百度学术中相似的文章 |
[Suo Y.]的文章 |
[Li S.]的文章 |
[Cao X.]的文章 |
必应学术 |
必应学术中相似的文章 |
[Suo Y.]的文章 |
[Li S.]的文章 |
[Cao X.]的文章 |
相关权益政策 |
暂无数据 |
收藏/分享 |
除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。