中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
首页 机构 成果 学者
  
  1. CAS IR Grid
  2. 地质与地球物理研究所
  3. 中国科学院地质与地球物理研究所
  4. 中国科学院新生代地质与环境重点实验室
The role of CO2 flushing in triggering the 'Millennium' eruption and recent unrests at Changbaishan volcano (China/North Korea)

文献类型：期刊论文

作者Pappalardo, Lucia1; Buono, Gianmarco1; Fanara, Sara2; Yi, Jian3; Shan, Xuanlong3; Guo, Zhengfu4; Zhang, Maoliang5; Ventura, Guido6,7
刊名INTERNATIONAL GEOLOGY REVIEW
出版日期2022-04-18
页码14
关键词Changbaishan volcano plumbing system modelling triggering mechanism CO2 flushing storage depth
ISSN号0020-6814
DOI10.1080/00206814.2022.2065544
英文摘要The impact of large-scale caldera-forming eruptions on our society and climate can be considerable. The triggering mechanisms of these eruptions and the instability of their magmatic systems are still elusive. Here we use X-ray tomographic microscopy, glass geochemistry and volatile element concentration data on the products of the 946 CE 'Millennium' eruption (ME) of Changbaishan volcano (China/North Korea) with the aim to identify the triggering mechanism of the eruption. ME emitted rhyolites and trachytes whose textural parameters suggest vesiculation events related to crystallization and magma ascent in the conduit, and to the arrival of new gas in the magmatic system. Solubility models show that the CO2 and H2O dissolved in the glass are consistent with a pressure of 100-200 MPa. Literature data from fluid inclusions in minerals indicate that the residing magma was CO2 free before the eruption, whereas the CO2 content in the glass reaches 600 ppm at the flash of the ME event. We find that a single, shallow magma reservoir localized between 7.5 and 3.7 km depth in which rhyolites occupies the top and trachytes the bottom is fully destabilized by the arrival of external CO2-rich fluids. Such fluids are released from a deeper, carbonate-rich mantle source. Our results and those of independent geophysical data show that the ME magmatic system is still active, and the continuous upraising of fluids from depth may drive unrest episodes like that recorded in 2002-2006. Our findings elucidate the role of deep, mantle-derived fluids in driving large-scale explosive eruptions. We provide evidence that volcanic unrests may not mirror the internal dynamics of magmatic reservoirs.
WOS关键词B-TM ERUPTION ; NORTHEAST CHINA ; TIANCHI VOLCANO ; SOLUBILITY ; EVOLUTION ; SYSTEM ; MAGMAS ; MELTS ; CONSTRAINTS ; NUCLEATION
资助项目INGV ; Chinese Academy of Sciences, Key Research Project of Frontier Sciences of Chinese Academy of Sciences, Natural Science Foundation of China
WOS研究方向Geology
语种英语
WOS记录号WOS:000783382200001
出版者TAYLOR & FRANCIS INC
资助机构INGV ; INGV ; Chinese Academy of Sciences, Key Research Project of Frontier Sciences of Chinese Academy of Sciences, Natural Science Foundation of China ; Chinese Academy of Sciences, Key Research Project of Frontier Sciences of Chinese Academy of Sciences, Natural Science Foundation of China ; INGV ; INGV ; Chinese Academy of Sciences, Key Research Project of Frontier Sciences of Chinese Academy of Sciences, Natural Science Foundation of China ; Chinese Academy of Sciences, Key Research Project of Frontier Sciences of Chinese Academy of Sciences, Natural Science Foundation of China ; INGV ; INGV ; Chinese Academy of Sciences, Key Research Project of Frontier Sciences of Chinese Academy of Sciences, Natural Science Foundation of China ; Chinese Academy of Sciences, Key Research Project of Frontier Sciences of Chinese Academy of Sciences, Natural Science Foundation of China ; INGV ; INGV ; Chinese Academy of Sciences, Key Research Project of Frontier Sciences of Chinese Academy of Sciences, Natural Science Foundation of China ; Chinese Academy of Sciences, Key Research Project of Frontier Sciences of Chinese Academy of Sciences, Natural Science Foundation of China
源URL[http://ir.iggcas.ac.cn/handle/132A11/105134]  
专题地质与地球物理研究所_中国科学院新生代地质与环境重点实验室
通讯作者Ventura, Guido
作者单位1.Ist Nazl Geofis & Vulcanol, Osservatorio Vesuviano Napoli, Naples, Italy
2.Georg August Univ Gottingen, Dept Expt & Appl Mineral, Gottingen, Germany
3.Jilin Univ, Coll Earth Sci, Changchun, Peoples R China
4.Chinese Acad Sci, Inst Geol & Geophys, Beijing, Peoples R China
5.Tianjin Univ, Sch Earth Syst Sci, Tianjin, Peoples R China
6.Ist Nazl Geofis & Vulcanol, Via Vigna Murata 605, I-00143 Rome, Italy
7.CNR, Ist Studio Impatti Antrop & Sostenibilita Ambient, Tp, Italy
推荐引用方式
GB/T 7714		 Pappalardo, Lucia,Buono, Gianmarco,Fanara, Sara,et al. The role of CO2 flushing in triggering the 'Millennium' eruption and recent unrests at Changbaishan volcano (China/North Korea)[J]. INTERNATIONAL GEOLOGY REVIEW,2022:14.
APA Pappalardo, Lucia.,Buono, Gianmarco.,Fanara, Sara.,Yi, Jian.,Shan, Xuanlong.,...&Ventura, Guido.(2022).The role of CO2 flushing in triggering the 'Millennium' eruption and recent unrests at Changbaishan volcano (China/North Korea).INTERNATIONAL GEOLOGY REVIEW,14.
MLA Pappalardo, Lucia,et al."The role of CO2 flushing in triggering the 'Millennium' eruption and recent unrests at Changbaishan volcano (China/North Korea)".INTERNATIONAL GEOLOGY REVIEW (2022):14.

入库方式： OAI收割

来源：地质与地球物理研究所

浏览0
下载0
收藏0
其他版本

除非特别说明，本系统中所有内容都受版权保护，并保留所有权利。