中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Growth and thermal maturation of the Toba magma reservoir

文献类型:期刊论文

作者Liu, Ping-Ping1,8,9; Caricchi, Luca2; Chung, Sun-Lin3,9; Li, Xian-Hua1; Li, Qiu-Li1; Zhou, Mei-Fu4; Lai, Yu-Ming7; Ghani, Azman A.5; Sihotang, Theodora6; Sheldrake, Tom E.2
刊名PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA
出版日期2021-11-09
卷号118期号:45页码:9
ISSN号0027-8424
关键词Toba caldera supereruption eruptible magma thermal modeling zircon
DOI10.1073/pnas.2101695118
英文摘要The Toba volcanic system in Indonesia has produced two of the largest eruptions (>2,000 km(3) dense-rock equivalent [DRE] each) on Earth since the Quaternary. U-Pb crystallization ages of zircon span a period of similar to 600 ky before each eruptive event, and in the run-up to each eruption, the mean and variance of the zircons' U content decrease. To quantify the process of accumulation of eruptible magma underneath the Toba caldera, we integrated these observations with thermal and geochemical modeling. We show that caldera-forming eruptions at Toba are the result of progressive thermal maturation of the upper crustal magma reservoir, which grows and chemically homogenizes, by sustained magma influx at average volumetric rates between 0.008 and 0.01 km(3)/y over the past 2.2 My. Protracted thermal pulses related to magma-recharge events prime the system for eruption without necessarily requiring an increased magma-recharge rate before the two supereruptions. If the rate of magma input was maintained since the last supereruption of Toba at 75 ka, eruptible magma is currently accumulating at a minimum rate of similar to 4.2 km(3) per millennium, and the current estimate of the total volume of potentially eruptible magma available today is a minimum of similar to 315 km(3). Our approach to evaluate magma flux and the rate of eruptible magma accumulation is applicable to other volcanic systems capable of producing supereruptions and thereby could help in assessing the potential of active volcanic systems to feed supereruptions.
WOS关键词U-PB ; ZIRCON ; TUFF ; GEOCHRONOLOGY ; SUMATRA ; STORAGE ; SIZE ; PETROGENESIS ; CONSTRAINTS ; EVOLUTION
资助项目Ministry of Science and Technology[106-2745-M-001-003-ASP] ; Chinese Academy of Sciences[XDB18030300] ; National Science Foundation of China[41872058] ; European Research Council under the European Union's Horizon 2020 Research and Innovation Program[677493] ; Swiss National Science Foundation
WOS研究方向Science & Technology - Other Topics
语种英语
出版者NATL ACAD SCIENCES
WOS记录号WOS:000720926900001
资助机构Ministry of Science and Technology ; Ministry of Science and Technology ; Ministry of Science and Technology ; Ministry of Science and Technology ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; National Science Foundation of China ; National Science Foundation of China ; National Science Foundation of China ; National Science Foundation of China ; European Research Council under the European Union's Horizon 2020 Research and Innovation Program ; European Research Council under the European Union's Horizon 2020 Research and Innovation Program ; European Research Council under the European Union's Horizon 2020 Research and Innovation Program ; European Research Council under the European Union's Horizon 2020 Research and Innovation Program ; Swiss National Science Foundation ; Swiss National Science Foundation ; Swiss National Science Foundation ; Swiss National Science Foundation ; Ministry of Science and Technology ; Ministry of Science and Technology ; Ministry of Science and Technology ; Ministry of Science and Technology ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; National Science Foundation of China ; National Science Foundation of China ; National Science Foundation of China ; National Science Foundation of China ; European Research Council under the European Union's Horizon 2020 Research and Innovation Program ; European Research Council under the European Union's Horizon 2020 Research and Innovation Program ; European Research Council under the European Union's Horizon 2020 Research and Innovation Program ; European Research Council under the European Union's Horizon 2020 Research and Innovation Program ; Swiss National Science Foundation ; Swiss National Science Foundation ; Swiss National Science Foundation ; Swiss National Science Foundation ; Ministry of Science and Technology ; Ministry of Science and Technology ; Ministry of Science and Technology ; Ministry of Science and Technology ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; National Science Foundation of China ; National Science Foundation of China ; National Science Foundation of China ; National Science Foundation of China ; European Research Council under the European Union's Horizon 2020 Research and Innovation Program ; European Research Council under the European Union's Horizon 2020 Research and Innovation Program ; European Research Council under the European Union's Horizon 2020 Research and Innovation Program ; European Research Council under the European Union's Horizon 2020 Research and Innovation Program ; Swiss National Science Foundation ; Swiss National Science Foundation ; Swiss National Science Foundation ; Swiss National Science Foundation ; Ministry of Science and Technology ; Ministry of Science and Technology ; Ministry of Science and Technology ; Ministry of Science and Technology ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; National Science Foundation of China ; National Science Foundation of China ; National Science Foundation of China ; National Science Foundation of China ; European Research Council under the European Union's Horizon 2020 Research and Innovation Program ; European Research Council under the European Union's Horizon 2020 Research and Innovation Program ; European Research Council under the European Union's Horizon 2020 Research and Innovation Program ; European Research Council under the European Union's Horizon 2020 Research and Innovation Program ; Swiss National Science Foundation ; Swiss National Science Foundation ; Swiss National Science Foundation ; Swiss National Science Foundation
源URL[http://ir.iggcas.ac.cn/handle/132A11/103839]  
专题地质与地球物理研究所_岩石圈演化国家重点实验室
通讯作者Liu, Ping-Ping; Caricchi, Luca; Chung, Sun-Lin
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China
2.Univ Geneva, Dept Earth Sci, CH-1205 Geneva, Switzerland
3.Natl Taiwan Univ, Dept Geosci, Taipei 10617, Taiwan
4.Chinese Acad Sci, Inst Geochem, State Key Lab Ore Deposit Geochem, Guiyang 550081, Peoples R China
5.Univ Malaya, Fac Sci, Dept Geol, Kuala Lumpur 50603, Malaysia
6.Samosir Geoarea Management Board, Toba Caldera Geopk, Samosir 22396, Indonesia
7.Natl Taiwan Normal Univ, Dept Earth Sci, Taipei 11677, Taiwan
8.Peking Univ, Sch Earth & Space Sci, Key Lab Orogen Belts & Crustal Evolut, Beijing 100871, Peoples R China
9.Acad Sinica, Inst Earth Sci, Taipei 11529, Taiwan
推荐引用方式
GB/T 7714
Liu, Ping-Ping,Caricchi, Luca,Chung, Sun-Lin,et al. Growth and thermal maturation of the Toba magma reservoir[J]. PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA,2021,118(45):9.
APA Liu, Ping-Ping.,Caricchi, Luca.,Chung, Sun-Lin.,Li, Xian-Hua.,Li, Qiu-Li.,...&Simpson, Guy.(2021).Growth and thermal maturation of the Toba magma reservoir.PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA,118(45),9.
MLA Liu, Ping-Ping,et al."Growth and thermal maturation of the Toba magma reservoir".PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA 118.45(2021):9.

入库方式: OAI收割

来源:地质与地球物理研究所

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