globalchange  > 过去全球变化的重建
DOI: 10.1371/journal.pone.0159200
论文题名:
The Year Leading to a Supereruption
作者: Guilherme A. R. Gualda; Stephen R. Sutton
刊名: PLOS ONE
ISSN: 1932-6203
出版年: 2016
发表日期: 2016-7-20
卷: 11, 期:7
语种: 英语
英文关键词: Quartz ; Crystallization ; Crystals ; Crystal growth ; Nucleation ; Relaxation time ; Scanning electron microscopy ; Laboratory glassware
英文摘要: Supereruptions catastrophically eject 100s-1000s of km3 of magma to the surface in a matter of days to a few months. In this study, we use zoning in quartz crystals from the Bishop Tuff (California) to assess the timescales over which a giant magma body transitions from relatively quiescent, pre-eruptive crystallization to rapid decompression and eruption. Quartz crystals in the Bishop Tuff have distinctive rims (<200 μm thick), which are Ti-rich and bright in cathodoluminescence (CL) images, and which can be used to calculate Ti diffusional relaxation times. We use synchrotron-based x-ray microfluorescence to obtain quantitative Ti maps and profiles along rim-interior contacts in quartz at resolutions of 1–5 μm in each linear dimension. We perform CL imaging on a scanning electron microscope (SEM) using a low-energy (5 kV) incident beam to characterize these contacts in high resolution (<1 μm in linear dimensions). Quartz growth times were determined using a 1D model for Ti diffusion, assuming initial step functions. Minimum quartz growth rates were calculated using these calculated growth times and measured rim thicknesses. Maximum rim growth times span from ~1 min to 35 years, with a median of ~4 days. More than 70% of rim growth times are less than 1 year, showing that quartz rims have mostly grown in the days to months prior to eruption. Minimum growth rates show distinct modes between 10−8 and 10−10 m/s (depending on sample), revealing very fast crystal growth rates (100s of nm to 10s of μm per day). Our data show that quartz rims grew well within a year of eruption, with most of the growth happening in the weeks or days preceding eruption. Growth took place under conditions of high supersaturation, suggesting that rim growth marks the onset of decompression and the transition from pre-eruptive to syn-eruptive conditions.
URL: http://journals.plos.org/plosone/article/file?id=10.1371/journal.pone.0159200&type=printable
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/23570
Appears in Collections:过去全球变化的重建
影响、适应和脆弱性
科学计划与规划
气候变化与战略
全球变化的国际研究计划
气候减缓与适应
气候变化事实与影响

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作者单位: Vanderbilt University, Earth & Environmental Sciences, PMB 351805, Nashville, TN, 37235, United States of America;University of Chicago, Department of Geophysical Sciences and Center for Advanced Radiation Sources, Chicago, IL, 60637, United States of America

Recommended Citation:
Guilherme A. R. Gualda,Stephen R. Sutton. The Year Leading to a Supereruption[J]. PLOS ONE,2016-01-01,11(7)
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