Gradual caldera collapse at Bardarbunga volcano, Iceland, regulated by lateral magma outflow

Gudmundsson Magnus T.; Jonsdottir Kristin; Hooper Andrew; Holohan Eoghan P.; Halldorsson Saemundur A.; Ofeigsson Benedikt G.; Cesca Simone; Vogfjord Kristin S.; Sigmundsson Freysteinn; Hognadottir Thordis; Einarsson Pall; Sigmarsson Olgeir; Jarosch Alexander H.; Jonasson Kristjan; Magnusson Eyjolfur; Hreinsdottir Sigrun; Bagnardi Marco; Parks Michelle M.; Hjorleifsdottir Vala; Palsson Finnur; Walter Thomas R.; Schopfer Martin P. J.; Heimann Sebastian; Reynolds Hannah I.; Dumont Stephanie; Bali Eniko; Gudfinnsson Gudmundur H.; Dahm Torsten; Roberts Matthew J.; Hensch Martin; Belart Joaquin M. C.; Spaans Karsten; Jakobsson Sigurdur; Gudmundsson Gunnar B.; Fridriksdottir Hildur M.; Drouin Vincent; Durig Tobias; Adalgeirsdottir Gudfinna; Riishuus Morten S.; Pedersen Gro B. M.; van Boeckel Tayo; Oddsson Bjorn; Pfeffer Melissa A.; Barsotti Sara; Bergsson Baldur; Donovan Amy; Burton Mike R.; Aiuppa Alessandro

首页> 外文期刊>Science >Gradual caldera collapse at Bardarbunga volcano, Iceland, regulated by lateral magma outflow

【24h】

Gradual caldera collapse at Bardarbunga volcano, Iceland, regulated by lateral magma outflow

机译：受横向岩浆流出的调节，冰岛Bardarbunga火山逐渐破火山口塌陷

获取原文

获取原文并翻译 | 示例

掌桥外文数据库（机构版） >>

开具论文收录证明 >>

文献代查 >>

页面导航

摘要
著录项
相似文献
相关主题

摘要

Large volcanic eruptions on Earth commonly occur with a collapse of the roof of a crustal magma reservoir, forming a caldera. Only a few such collapses occur per century, and the lack of detailed observations has obscured insight into the mechanical interplay between collapse and eruption. We use multiparameter geophysical and geochemical data to show that the 110-square-kilometer and 65-meter-deep collapse of Bardarbunga caldera in 2014-2015 was initiated through withdrawal of magma, and lateral migration through a 48-kilometers-long dike, from a 12-kilometers deep reservoir. Interaction between the pressure exerted by the subsiding reservoir roof and the physical properties of the subsurface flow path explain the gradual, near-exponential decline of both collapse rate and the intensity of the 180-day-long eruption.

机译：地球上的大型火山喷发通常发生在地壳岩浆储层的屋顶坍塌，形成火山口。每个世纪仅发生了几次这样的坍塌，并且由于缺乏详细的观察，使得人们对坍塌和喷发之间的机械相互作用的见解变得模糊。我们使用多参数地球物理和地球化学数据显示，2014-2015年Bardarbunga破火山口的110平方公里和65米深的塌陷是通过岩浆撤离以及通过48公里长的堤坝的横向迁移而引起的。一个12公里深的水库。塌陷的储层顶板施加的压力与地下流路的物理特性之间的相互作用解释了塌陷率和180天喷发强度的逐渐接近指数级下降。

著录项

来源
《Science》 |2016年第6296期|262-262|共1页
作者
Gudmundsson Magnus T.; Jonsdottir Kristin; Hooper Andrew; Holohan Eoghan P.; Halldorsson Saemundur A.; Ofeigsson Benedikt G.; Cesca Simone; Vogfjord Kristin S.; Sigmundsson Freysteinn; Hognadottir Thordis; Einarsson Pall; Sigmarsson Olgeir; Jarosch Alexander H.; Jonasson Kristjan; Magnusson Eyjolfur; Hreinsdottir Sigrun; Bagnardi Marco; Parks Michelle M.; Hjorleifsdottir Vala; Palsson Finnur; Walter Thomas R.; Schopfer Martin P. J.; Heimann Sebastian; Reynolds Hannah I.; Dumont Stephanie; Bali Eniko; Gudfinnsson Gudmundur H.; Dahm Torsten; Roberts Matthew J.; Hensch Martin; Belart Joaquin M. C.; Spaans Karsten; Jakobsson Sigurdur; Gudmundsson Gunnar B.; Fridriksdottir Hildur M.; Drouin Vincent; Durig Tobias; Adalgeirsdottir Gudfinna; Riishuus Morten S.; Pedersen Gro B. M.; van Boeckel Tayo; Oddsson Bjorn; Pfeffer Melissa A.; Barsotti Sara; Bergsson Baldur; Donovan Amy; Burton Mike R.; Aiuppa Alessandro;
展开▼
作者单位

Univ Iceland, Nordvulk Inst Earth Sci, Sturlugata 7, IS-101 Reykjavik, Iceland;

Iceland Meteorol Off, IS-150 Reykjavik, Iceland;

Univ Leeds, Ctr Observat & Modelling Earthquakes Volcanoes &, Sch Earth & Environm, Leeds LS2 9JT, W Yorkshire, England;

GFZ German Res Ctr Geosci, D-14473 Potsdam, Germany|Univ Coll Dublin, Sch Earth Sci, Dublin, Ireland;

Univ Iceland, Nordvulk Inst Earth Sci, Sturlugata 7, IS-101 Reykjavik, Iceland;

Iceland Meteorol Off, IS-150 Reykjavik, Iceland;

GFZ German Res Ctr Geosci, D-14473 Potsdam, Germany;

Iceland Meteorol Off, IS-150 Reykjavik, Iceland;

Univ Iceland, Nordvulk Inst Earth Sci, Sturlugata 7, IS-101 Reykjavik, Iceland;

Univ Iceland, Nordvulk Inst Earth Sci, Sturlugata 7, IS-101 Reykjavik, Iceland;

Univ Iceland, Nordvulk Inst Earth Sci, Sturlugata 7, IS-101 Reykjavik, Iceland;

Univ Iceland, Nordvulk Inst Earth Sci, Sturlugata 7, IS-101 Reykjavik, Iceland|Univ Clermont Ferrand, IRD, Lab Magmas & Volcans, F-63038 Clermont Ferrand, France;

Univ Iceland, Nordvulk Inst Earth Sci, Sturlugata 7, IS-101 Reykjavik, Iceland;

Univ Iceland, Fac Ind & Mech Engn & Comp Sci, Hjardarhagi 2-6, IS-107 Reykjavik, Iceland;

Univ Iceland, Nordvulk Inst Earth Sci, Sturlugata 7, IS-101 Reykjavik, Iceland;

GNS Sci, POB 30368, Lower Hutt 5040, New Zealand;

Univ Iceland, Nordvulk Inst Earth Sci, Sturlugata 7, IS-101 Reykjavik, Iceland;

Univ Nacl Autonoma Mexico, Dept Sismol, Inst Geofis, Mexico City 04510, DF, Mexico;

Univ Iceland, Nordvulk Inst Earth Sci, Sturlugata 7, IS-101 Reykjavik, Iceland;

GFZ German Res Ctr Geosci, D-14473 Potsdam, Germany;

Univ Vienna, Dept Geodynam & Sedimentol, Althanstr 14, A-1090 Vienna, Austria;

GFZ German Res Ctr Geosci, D-14473 Potsdam, Germany;

Univ Iceland, Nordvulk Inst Earth Sci, Sturlugata 7, IS-101 Reykjavik, Iceland;

Univ Iceland, Nordvulk Inst Earth Sci, Sturlugata 7, IS-101 Reykjavik, Iceland;

Univ Iceland, Nordvulk Inst Earth Sci, Sturlugata 7, IS-101 Reykjavik, Iceland;

Univ Iceland, Nordvulk Inst Earth Sci, Sturlugata 7, IS-101 Reykjavik, Iceland;

GFZ German Res Ctr Geosci, D-14473 Potsdam, Germany;

Iceland Meteorol Off, IS-150 Reykjavik, Iceland;

Iceland Meteorol Off, IS-150 Reykjavik, Iceland;

Univ Iceland, Nordvulk Inst Earth Sci, Sturlugata 7, IS-101 Reykjavik, Iceland;

Univ Leeds, Ctr Observat & Modelling Earthquakes Volcanoes &, Sch Earth & Environm, Leeds LS2 9JT, W Yorkshire, England;

Univ Iceland, Nordvulk Inst Earth Sci, Sturlugata 7, IS-101 Reykjavik, Iceland;

Iceland Meteorol Off, IS-150 Reykjavik, Iceland;

Univ Iceland, Nordvulk Inst Earth Sci, Sturlugata 7, IS-101 Reykjavik, Iceland|Iceland Meteorol Off, IS-150 Reykjavik, Iceland;

Univ Iceland, Nordvulk Inst Earth Sci, Sturlugata 7, IS-101 Reykjavik, Iceland;

Univ Iceland, Nordvulk Inst Earth Sci, Sturlugata 7, IS-101 Reykjavik, Iceland|Natl Commissioner Iceland Police, Dept Civil Protect & Emergency Management, Skulagata 21, IS-101 Reykjavik, Iceland;

Univ Iceland, Nordvulk Inst Earth Sci, Sturlugata 7, IS-101 Reykjavik, Iceland;

Univ Iceland, Nordvulk Inst Earth Sci, Sturlugata 7, IS-101 Reykjavik, Iceland;

Univ Iceland, Nordvulk Inst Earth Sci, Sturlugata 7, IS-101 Reykjavik, Iceland;

Univ Iceland, Nordvulk Inst Earth Sci, Sturlugata 7, IS-101 Reykjavik, Iceland;

Natl Commissioner Iceland Police, Dept Civil Protect & Emergency Management, Skulagata 21, IS-101 Reykjavik, Iceland;

Iceland Meteorol Off, IS-150 Reykjavik, Iceland;

Iceland Meteorol Off, IS-150 Reykjavik, Iceland;

Iceland Meteorol Off, IS-150 Reykjavik, Iceland;

Kings Coll London, Kings Bldg,Strand Campus, London WC2R 2LS, England;

Univ Manchester, Williamson Bldg,Oxford Rd, Manchester M13 9PL, Lancs, England;

Univ Manchester, Williamson Bldg,Oxford Rd, Manchester M13 9PL, Lancs, England;

展开▼
收录信息美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);美国《化学文摘》(CA);
原文格式 PDF
正文语种 eng
中图分类
关键词

相似文献

外文文献
中文文献

1. Magma interactions, crystal mush formation, timescales, and unrest during caldera collapse and lateral eruption at ocean island basaltic volcanoes (Piton de la Fournaise, La Reunion) [J] . Albert H., Costa E., Di Muro A., Earth and Planetary Science Letters: A Letter Journal Devoted to the Development in Time of the Earth and Planetary System . 2019,第期

机译：Magma互动，水晶糊状形成，时间尺度，在海岛玄武岩火山（Piton de la Fournaise）的海岛坍塌和侧爆发期间，突然爆发
2. Formation of OEskjuvatn caldera at Askja, North Iceland: Mechanism of caldera collapse and implications for the lateral flow hypothesis [J] . M.E. Hartley, T. Thordarson Journal of Volcanology and Geothermal Research . 2012,第Maya15期

机译：冰岛北部Askja OEskjuvatn破火山口的形成：破火山口塌陷的机理及其对侧向流动假设的影响
3. How summit calderas collapse on basaltic volcanoes: New insights from the April 2007 caldera collapse of Piton de la Fournaise volcano [J] . Laurent Michon, Nicolas Villeneuve, Thibault Catry, Journal of Volcanology and Geothermal Research . 2009,第1a2期

机译：峰顶破火山口如何在玄武质火山上坍塌：Piton de la Fournaise火山2007年4月破火山口塌陷的新发现
4. DEFORMATION DUE TO MAGMA MOVEMENT AND ICE UNLOADING AT KATLA VOLCANO, ICELAND, DETECTED BY PERSISTENT SCATTERER INSAR [C] . Andrew Hooper, Rikke Pedersen Envisat Symposium . 2007

机译：由于岩浆火山，冰岛的岩浆运动和冰块因岩浆而卸载而变形，由持久散射体insar检测到
5. Magma dynamics inferred from feldspar zoning in post-caldera phonolites, Suswa Volcano, Kenya Rift, Africa. [D] . Espejel-Garcia, Vanessa Veronica. 2006

机译：从非洲肯尼亚裂谷苏斯瓦火山火山口后的长石中的长石地带推断出岩浆动力学。
6. Crustal movements due to Iceland’s shrinking ice caps mimic magma inflow signal at Katla volcano [O] . Karsten Spaans, Sigrún Hreinsdóttir, Andrew Hooper, -1

机译：由于冰岛的冰盖缩小模拟了卡特拉火山的岩浆流入信号导致地壳运动
7. Gradual caldera collapse at Bárdarbunga volcano, Iceland, regulated by lateral magma outflow [O] . Gudmundsson, Magnús, Jónsdóttir, Kristín, Hooper, Andrew, 2016

机译：受横向岩浆流出的调节，冰岛巴尔达邦加火山的火山口逐渐塌陷
8. Seismological evidence for Lateral magma intrusion during the July 1978 deflation of the Krafla volcano in NE-Iceland [R] . 1978

机译：1978年7月东北冰岛克拉夫拉火山放气期间侧向岩浆侵入的地震证据

Gradual caldera collapse at Bardarbunga volcano, Iceland, regulated by lateral magma outflow

摘要

著录项

相似文献

相关主题

期刊订阅