Voluminous eruption from a zoned magma body after an increase in supply rate at Axial Seamount

被引:60
|
作者
Chadwick, W. W., Jr. [1 ]
Paduan, J. B. [2 ]
Clague, D. A. [2 ]
Dreyer, B. M. [3 ]
Merle, S. G. [1 ]
Bobbitt, A. M. [1 ]
Caress, D. W. [2 ]
Philip, B. T. [4 ]
Kelley, D. S. [4 ]
Nooner, S. L. [5 ]
机构
[1] Oregon State Univ, Hatfield Marine Sci Ctr, CIMRS, Newport, OR 97365 USA
[2] Monterey Bay Aquarium Res Inst, Moss Landing, CA USA
[3] Univ Santa Cruz, Dept Earth & Planetary Sci, Santa Cruz, CA USA
[4] Univ Washington, Sch Oceanog, Seattle, WA 98195 USA
[5] Univ North Carolina Wilmington, Wilmington, NC USA
基金
美国国家科学基金会; 美国海洋和大气管理局;
关键词
submarine eruption; basaltic caldera; lava emplacement; mid-ocean ridge; dike intrusion; rift zone; HIGH-RESOLUTION; LAVA FLOW; VOLCANO; SUMMIT; EMPLACEMENT; CONSTRAINTS;
D O I
10.1002/2016GL071327
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Axial Seamount is the best monitored submarine volcano in the world, providing an exceptional window into the dynamic interactions between magma storage, transport, and eruption processes in a mid-ocean ridge setting. An eruption in April 2015 produced the largest volume of erupted lava since monitoring and mapping began in the mid-1980s after the shortest repose time, due to a recent increase in magma supply. The higher rate of magma replenishment since 2011 resulted in the eruption of the most mafic lava in the last 500-600years. Eruptive fissures at the volcano summit produced pyroclastic ash that was deposited over an area of at least 8km(2). A systematic spatial distribution of compositions is consistent with a single dike tapping different parts of a thermally and chemically zoned magma reservoir that can be directly related to previous multichannel seismic-imaging results.
引用
收藏
页码:12063 / 12070
页数:8
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