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DOI | 10.1038/s41467-020-16521-0 |
Geophysical imaging of ophiolite structure in the United Arab Emirates | |
M. Y. Ali; A. B. Watts; M. P. Searle; B. Keats; S. Pilia; T. Ambrose | |
2020-05-29 | |
发表期刊 | Nature Communications |
出版年 | 2020 |
英文摘要 | AbstractThe Oman-United Arab Emirates ophiolite has been used extensively to document the geological processes that form oceanic crust. The geometry of the ophiolite, its extension into the Gulf of Oman, and the nature of the crust that underlies it are, however, unknown. Here, we show the ophiolite forms a high velocity, high density, >15鈥塳m thick east-dipping body that during emplacement flexed down a previously rifted continental margin thereby contributing to subsidence of flanking sedimentary basins. The western limit of the ophiolite is defined onshore by the Semail thrust while the eastern limit extends several km offshore, where it is defined seismically by a ~40鈥?5掳, east-dipping, normal fault. The fault is interpreted as the southwestern margin of an incipient suture zone that separates the Arabian plate from in situ Gulf of Oman oceanic crust and mantle presently subducting northwards beneath the Eurasian plate along the Makran trench. |
领域 | 资源环境 |
URL | 查看原文 |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://119.78.100.173/C666/handle/2XK7JSWQ/271698 |
专题 | 资源环境科学 |
推荐引用方式 GB/T 7714 | M. Y. Ali,A. B. Watts,M. P. Searle,et al. Geophysical imaging of ophiolite structure in the United Arab Emirates[J]. Nature Communications,2020. |
APA | M. Y. Ali,A. B. Watts,M. P. Searle,B. Keats,S. Pilia,&T. Ambrose.(2020).Geophysical imaging of ophiolite structure in the United Arab Emirates.Nature Communications. |
MLA | M. Y. Ali,et al."Geophysical imaging of ophiolite structure in the United Arab Emirates".Nature Communications (2020). |
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