Rapid onset of mafic magmatism facilitated by volcanic edifice collapse
文献类型:期刊论文
作者 | Cassidy, M.1,2; Watt, S. F. L.1,3; Talling, P. J.4; Palmer, M. R.1; Edmonds, M.5; Jutzeler, M.4; Wall-Palmer, D.6; Manga, M.7; Coussens, M.4; Gernon, T.1 |
刊名 | GEOPHYSICAL RESEARCH LETTERS
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出版日期 | 2015-06-28 |
卷号 | 42期号:12页码:4778-4785 |
关键词 | Sector Collapse Clinopyroxene Petrology Magma Ascent |
DOI | 10.1002/2015GL064519 |
文献子类 | Article |
英文摘要 | Volcanic edifice collapses generate some of Earth's largest landslides. How such unloading affects the magma storage systems is important for both hazard assessment and for determining long-term controls on volcano growth and decay. Here we present a detailed stratigraphic and petrological analyses of volcanic landslide and eruption deposits offshore Montserrat, in a subduction zone setting, sampled during Integrated Ocean Drilling Program Expedition 340. A large (6-10km(3)) collapse of the Soufriere Hills Volcano at similar to 130ka was followed by explosive basaltic volcanism and the formation of a new basaltic volcanic center, the South Soufriere Hills, estimated to have initiated <100years after collapse. This basaltic volcanism was a sharp departure from the andesitic volcanism that characterized Soufriere Hills' activity before the collapse. Mineral-melt thermobarometry demonstrates that the basaltic magma's transit through the crust was rapid and from midcrustal depths. We suggest that this rapid ascent was promoted by unloading following collapse. |
WOS关键词 | SOUFRIERE HILLS VOLCANO ; LESSER ANTILLES ; AMPHIBOLE SPONGE ; FLANK-COLLAPSE ; ARC CRUST ; MONTSERRAT ; EVOLUTION ; ERUPTION ; CONSEQUENCES ; CHAMBERS |
WOS研究方向 | Geology |
语种 | 英语 |
WOS记录号 | WOS:000358002500017 |
资助机构 | NERC(NE/K000403/1) ; NERC(NE/K000403/1) ; Alexander Von Humboldt fellowship ; Alexander Von Humboldt fellowship ; (NE/K002724/1) ; (NE/K002724/1) ; NERC(NE/K000403/1) ; NERC(NE/K000403/1) ; Alexander Von Humboldt fellowship ; Alexander Von Humboldt fellowship ; (NE/K002724/1) ; (NE/K002724/1) |
源URL | [http://ir.iggcas.ac.cn/handle/132A11/62323] ![]() |
专题 | 地质与地球物理研究所_其他部门 |
作者单位 | 1.Univ Southampton, Ocean & Earth Sci, Southampton, Hants, England 2.Johannes Gutenberg Univ Mainz, Inst Geosci, D-55122 Mainz, Germany 3.Univ Birmingham, Sch Geog Earth & Environm Sci, Birmingham, W Midlands, England 4.Natl Oceanog Ctr, Marine Geosci, Southampton, Hants, England 5.Univ Cambridge, Dept Earth Sci, Cambridge CB2 3EQ, England 6.Univ Plymouth, Sch Geog Earth & Environm Sci, Plymouth PL4 8AA, Devon, England 7.Univ Calif Berkeley, Dept Earth & Planetary Sci, Berkeley, CA 94720 USA 8.Tech Univ Bergakad Freiberg, Inst Geol & Palaontol, D-09596 Freiberg, Germany 9.CNRS, Sorbonne Paris Cite, UMR 7154, Equipe Geol Syst Volcan,Inst Phys Globe Paris, Paris, France 10.Geol Survey Japan AIST, Tsukuba, Ibaraki, Japan |
推荐引用方式 GB/T 7714 | Cassidy, M.,Watt, S. F. L.,Talling, P. J.,et al. Rapid onset of mafic magmatism facilitated by volcanic edifice collapse[J]. GEOPHYSICAL RESEARCH LETTERS,2015,42(12):4778-4785. |
APA | Cassidy, M..,Watt, S. F. L..,Talling, P. J..,Palmer, M. R..,Edmonds, M..,...&Wang, F..(2015).Rapid onset of mafic magmatism facilitated by volcanic edifice collapse.GEOPHYSICAL RESEARCH LETTERS,42(12),4778-4785. |
MLA | Cassidy, M.,et al."Rapid onset of mafic magmatism facilitated by volcanic edifice collapse".GEOPHYSICAL RESEARCH LETTERS 42.12(2015):4778-4785. |
入库方式: OAI收割
来源:地质与地球物理研究所
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