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DOI | 10.1029/2019JB018873 |
Dynamics of the Gibraltar Arc System: A Complex Interaction Between Plate Convergence, Slab Pull, and Mantle Flow | |
Civiero C.; Custódio S.; Duarte J.C.; Mendes V.B.; Faccenna C. | |
发表日期 | 2020 |
ISSN | 21699313 |
卷号 | 125期号:7 |
英文摘要 | In typical subduction systems, plate convergence is subperpendicular to the trench. The Gibraltar Arc System is exceptional, with its narrow subduction arc oriented N-S and laterally “squeezed” by the NNW-SSE tectonic convergence between Nubia and Iberia. The extent to which the slab is still coupled to the surface and how it interacts actively with the surrounding mantle is a matter of ongoing debate. Here, we analyze new densely spaced GPS data, together with crustal and mantle observations, to better understand the slab kinematics, plate dynamics, and mantle flow. In light of previous and current research, we find that subduction below the Gibraltar Arc is currently in the middle of a disruption process, with parts of it already detached and others yet coupled to the surface. In particular, the slab seems to be detached to the north of the Gibraltar Strait, with a small portion still attached to the surface or in the process of detaching below the western Betics. South of Gibraltar, the slab is still coupled to the overriding plate, although the subduction seems to be very slow or stopped. Flow of mantle material around the detached portions of the slab causes most of the surface uplift and a positive residual topography anomaly. Our findings show that the interplay between slab dynamics, mantle flow, and plate convergence explains much of the observed residual topography, surface motion, seismicity, and mantle structure. ©2020. American Geophysical Union. All Rights Reserved. |
英文关键词 | Gibraltar Arc; mantle flow; plate convergence; slab pull; subduction zone; surface deformation |
语种 | 英语 |
来源期刊 | Journal of Geophysical Research: Solid Earth
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文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/187764 |
作者单位 | Geophysics Section, Dublin Institute for Advanced Studies (DIAS), Dublin, Ireland; Instituto Dom Luiz (IDL), Faculdade de Ciências, Universidade de Lisboa, Lisbon, Portugal; Departamento de Geologia, Faculdade de Ciências, Universidade de Lisboa, Lisbon, Portugal; School of Earth, Atmosphere and Environment, Monash University, Melbourne, VIC, Australia; Dipartimento di Scienze Geologiche, Università di Roma Tre, Rome, Italy |
推荐引用方式 GB/T 7714 | Civiero C.,Custódio S.,Duarte J.C.,et al. Dynamics of the Gibraltar Arc System: A Complex Interaction Between Plate Convergence, Slab Pull, and Mantle Flow[J],2020,125(7). |
APA | Civiero C.,Custódio S.,Duarte J.C.,Mendes V.B.,&Faccenna C..(2020).Dynamics of the Gibraltar Arc System: A Complex Interaction Between Plate Convergence, Slab Pull, and Mantle Flow.Journal of Geophysical Research: Solid Earth,125(7). |
MLA | Civiero C.,et al."Dynamics of the Gibraltar Arc System: A Complex Interaction Between Plate Convergence, Slab Pull, and Mantle Flow".Journal of Geophysical Research: Solid Earth 125.7(2020). |
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