Ring faulting and piston collapse in the mantle sustained the largest submarine eruption ever documented

IF 4.8 1区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS Earth and Planetary Science Letters Pub Date : 2024-10-11 DOI:10.1016/j.epsl.2024.119026
E. Jacques , R. Hoste-Colomer , N. Feuillet , A. Lemoine , J. van der Woerd , W.C. Crawford , C. Berthod , P. Bachèlery
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Abstract

The basaltic submarine eruption offshore the island of Mayotte between July 2018 and January 2021 is one of the largest documented underwater eruptions. One of the most striking differences between this eruption and most documented eruptions is the exceptional depth of the associated seismicity, which is limited almost exclusively to the lithospheric mantle. This seismicity probably outlines magma reservoirs and dyking zones.
In order to better understand the deep processes driving the eruption, we analyze precise earthquake locations and focal mechanisms associated with this event. We present a set of 2677 accurate earthquake relocations and 300 focal mechanisms determined from data collected over the first 9 months of ocean bottom seismometer deployments, starting in February 2019.
Our relocations refine the structure of two swarms (Proximal and Distal with respect to Mayotte), and reveal well-defined mantle structures between 20 and 55 km below sea level, which we interpret as a ring-fault zone and a dyke, respectively. The Proximal swarm outlines a ring-fault zone as the locus of a large piston collapse caused by the deflation of an underlying magma reservoir. Deformation around the piston is driven by normal faulting on a set of inward dipping patches surrounding the piston. Locally, collapse of the conical shaped piston causes a radial extensional stress field with strike-slip and normal faulting ruptures accommodating the relaxation of the damaged zone around the piston.
This piston collapse allowed the transfer of lava to the eruption site via the dyke highlighted by the Distal earthquake swarm. The link between the swarms is thus magmatic, in agreement with petrological analyses of lava from the new volcano.
This is the first time that piston collapse and localized dyking have been documented in the mantle. The pattern of deformation documented here could apply to shallower, crustal piston collapses, such as in Iceland.
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地幔中的环状断层和活塞塌陷维持了有史以来最大的海底火山爆发
2018 年 7 月至 2021 年 1 月间马约特岛近海的玄武岩海底喷发是有记录的最大水下喷发之一。这次喷发与大多数记录在案的喷发之间最显著的区别之一是相关地震的深度特别大,几乎只限于岩石圈地幔。为了更好地了解驱动此次喷发的深层过程,我们分析了与此次事件相关的精确地震位置和聚焦机制。我们从 2019 年 2 月开始,通过前 9 个月的海底地震仪部署所收集的数据,确定了一组 2677 次精确地震定位和 300 个焦点机制。我们的定位完善了两个震群(相对于马约特岛的近端震群和远端震群)的结构,并揭示了海平面以下 20 至 55 千米之间定义明确的地幔结构,我们将其分别解释为环状断层带和堤坝。近端岩浆群勾勒出的环状断层带是一个大型活塞塌陷的位置,该活塞塌陷是由地下岩浆储层的膨胀引起的。活塞周围的变形是由活塞周围一组向内倾斜的斑块上的正断层驱动的。在局部,锥形活塞的坍塌造成了径向伸展应力场,而走向滑动和正断层的断裂适应了活塞周围受损区域的松弛。因此,地震群之间的联系是岩浆作用,这与新火山熔岩的岩石学分析结果一致。这里记录的变形模式可能适用于较浅的地壳活塞塌陷,如冰岛的活塞塌陷。
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来源期刊
Earth and Planetary Science Letters
Earth and Planetary Science Letters 地学-地球化学与地球物理
CiteScore
10.30
自引率
5.70%
发文量
475
审稿时长
2.8 months
期刊介绍: Earth and Planetary Science Letters (EPSL) is a leading journal for researchers across the entire Earth and planetary sciences community. It publishes concise, exciting, high-impact articles ("Letters") of broad interest. Its focus is on physical and chemical processes, the evolution and general properties of the Earth and planets - from their deep interiors to their atmospheres. EPSL also includes a Frontiers section, featuring invited high-profile synthesis articles by leading experts on timely topics to bring cutting-edge research to the wider community.
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