globalchange  > 过去全球变化的重建
DOI: 10.1371/journal.pone.0113157
论文题名:
Localized Rejuvenation of a Crystal Mush Recorded in Zircon Temporal and Compositional Variation at the Lassen Volcanic Center, Northern California
作者: Erik W. Klemetti; Michael A. Clynne
刊名: PLOS ONE
ISSN: 1932-6203
出版年: 2014
发表日期: 2014-12-3
卷: 9, 期:12
语种: 英语
英文关键词: Crystals ; Volcanoes ; Crystallization ; Crystalline inclusions ; Lakes ; Trace elements ; Quartz ; Planetary geology
英文摘要: Zircon ages and trace element compositions from recent silicic eruptions in the Lassen Volcanic Center (LVC) allow for an evaluation of the timing and conditions of rejuvenation (reheating and mobilization of crystals) within the LVC magmatic system. The LVC is the southernmost active Cascade volcano and, prior to the 1980 eruption of Mount St. Helens, was the site of the only eruption in the Cascade arc during the last century. The three most recent silicic eruptions from the LVC were very small to moderate-sized lava flows and domes of dacite (1915 and 27 ka eruptions of Lassen Peak) and rhyodacite (1.1 ka eruption of Chaos Crags). These eruptions produced mixed and mingled lavas that contain a diverse crystal cargo, including zircon. 238U-230Th model ages from interior and surface analyses of zircon reveal ages from ∼17 ka to secular equilibrium (>350 ka), with most zircon crystallizing during a period between ∼60–200 ka. These data support a model for localized rejuvenation of crystal mush beneath the LVC. This crystal mush evidently is the remnant of magmatism that ended ∼190 ka. Most zircon are thought to have been captured from “cold storage” in the crystal mush (670–725°C, Hf >10,000 ppm, Eu/Eu* 0.25–0.4) locally remobilized by intrusion of mafic magma. A smaller population of zircon (>730°C, Hf <10,000 ppm, Eu/Eu* >0.4) grew in, and are captured from, rejuvenation zones. These data suggest the dominant method to produce eruptible melt within the LVC is small-scale, local rejuvenation of the crystal mush accompanied by magma mixing and mingling. Based on zircon stability, the time required to heat, erupt and then cool to background conditions is relatively short, lasting a maximum of 10 s–1000 s years. Rejuvenation events in the LVC are ephemeral and permit eruption within an otherwise waning and cooling magmatic body.
URL: http://journals.plos.org/plosone/article/file?id=10.1371/journal.pone.0113157&type=printable
Citation statistics:
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/17768
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

Files in This Item:
File Name/ File Size Content Type Version Access License
journal.pone.0113157.PDF(9424KB)期刊论文作者接受稿开放获取View Download

作者单位: Department of Geosciences, Denison University, Granville OH 43023, United States of America;U.S. Geological Survey, Volcano Science Center, Menlo Park CA 94025, United States of America

Recommended Citation:
Erik W. Klemetti,Michael A. Clynne. Localized Rejuvenation of a Crystal Mush Recorded in Zircon Temporal and Compositional Variation at the Lassen Volcanic Center, Northern California[J]. PLOS ONE,2014-01-01,9(12)
Service
Recommend this item
Sava as my favorate item
Show this item's statistics
Export Endnote File
Google Scholar
Similar articles in Google Scholar
[Erik W. Klemetti]'s Articles
[Michael A. Clynne]'s Articles
百度学术
Similar articles in Baidu Scholar
[Erik W. Klemetti]'s Articles
[Michael A. Clynne]'s Articles
CSDL cross search
Similar articles in CSDL Cross Search
[Erik W. Klemetti]‘s Articles
[Michael A. Clynne]‘s Articles
Related Copyright Policies
Null
收藏/分享
文件名: journal.pone.0113157.PDF
格式: Adobe PDF
此文件暂不支持浏览
所有评论 (0)
暂无评论
 

Items in IR are protected by copyright, with all rights reserved, unless otherwise indicated.