U-series zircon age constraints on the plumbing system and magma residence times of the Changbai volcano, China/North Korea border | |
Zou, Haibo1; Fan, Qicheng2; Zhang, Hongfu3; Schmitt, Axel K.4 | |
刊名 | LITHOS
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2014-07-01 | |
卷号 | 200页码:169-180 |
关键词 | Changbai volcano Young zircons U-series disequilibrium Magma plumbing system Magma residence times |
ISSN号 | 0024-4937 |
DOI | 10.1016/j.lithos.2014.04.020 |
文献子类 | Article |
英文摘要 | The Changbai (or Baitoushan, Paektu) volcano on the China/North Korea border is best known for its climactic caldera-forming eruption of 100 km(3) of comendite materials 1000 years (1 ka) ago. The polygenetic Changbai volcano also erupted moderate-volume pre-caldera comendite lava at similar to 4 ka and small-volume post-caldera trachyte ignimbrite at similar to 0.3 ka. Here we report U-238-Th-230 disequilibrium ages of zircons from lavas and ignimbrites of the pre-caldera (similar to 4 ka), syn-caldera (1 ka), and post-caldera (similar to 0.3 ka) events. The zircon isochron ages are 12.2 +/- 1.1 ka (2 sigma) for the 4-ka comendite lava and 12.2 +/- 1.7 ka for the 1-ka comendite ignimbrite. Zircons from the 0.3-ka trachyte ignimbrite exhibit 3 respective peaks at 2.6 +/- 1.8 ka, 130 +/- 10 ka and >230 ka. The indistinguishable zircon ages for the 4-ka pre-caldera eruption of comendite lava and the 1-ka caldera-forming eruption of comendite pumice and ignimbrite suggest that the 4-ka lava provides an early sampling of a much larger magma body at depth and thus serves as a kind of petrologic early-warning signal. In addition, the 4-ka lava may represent the lowest-temperature magma in the roof zone of a thermally zoned magma chamber that usually escapes first. The distinctive multi-modal zircon age distributions of the 0.3-ka trachytic eruption, however, reveal that this post-caldera eruption tapped a different magma body and indicate that Changbai's magmatic plumbing system had changed after the 1-ka caldera-forming climactic eruption. Our results suggest very short zircon and magma residence times for the Changbai volcano (8 kyr for the 4-ka eruption, 11-12 kyr for the 1-ka eruption and 2.3 kyr for the 0.3-ka eruption). (C) 2014 Elsevier B.V. All rights reserved. |
WOS关键词 | TIANCHI VOLCANO ; NORTHEAST CHINA ; LONG VALLEY ; NEW-ZEALAND ; TRACE-ELEMENT ; MAJOR-ELEMENT ; CRATER LAKE ; JAPAN SEA ; TH-PB ; ERUPTION |
WOS研究方向 | Geochemistry & Geophysics ; Mineralogy |
语种 | 英语 |
出版者 | ELSEVIER SCIENCE BV |
WOS记录号 | WOS:000338810700012 |
资助机构 | US NSF(EAR-1119077) ; US NSF(EAR-1119077) ; NSF Earth Sciences Instrumentation and Facility program ; NSF Earth Sciences Instrumentation and Facility program ; US NSF(EAR-1119077) ; US NSF(EAR-1119077) ; NSF Earth Sciences Instrumentation and Facility program ; NSF Earth Sciences Instrumentation and Facility program ; US NSF(EAR-1119077) ; US NSF(EAR-1119077) ; NSF Earth Sciences Instrumentation and Facility program ; NSF Earth Sciences Instrumentation and Facility program ; US NSF(EAR-1119077) ; US NSF(EAR-1119077) ; NSF Earth Sciences Instrumentation and Facility program ; NSF Earth Sciences Instrumentation and Facility program |
内容类型 | 期刊论文 |
源URL | [http://ir.iggcas.ac.cn/handle/132A11/86422] ![]() |
专题 | 中国科学院地质与地球物理研究所 |
通讯作者 | Zou, Haibo |
作者单位 | 1.Auburn Univ, Dept Geol & Geog, Auburn, AL 36849 USA 2.China Earthquake Adm, Inst Geol, Beijing 100029, Peoples R China 3.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China 4.Univ Calif Los Angeles, Dept Earth & Space Sci, Los Angeles, CA 90095 USA |
推荐引用方式 GB/T 7714 | Zou, Haibo,Fan, Qicheng,Zhang, Hongfu,et al. U-series zircon age constraints on the plumbing system and magma residence times of the Changbai volcano, China/North Korea border[J]. LITHOS,2014,200:169-180. |
APA | Zou, Haibo,Fan, Qicheng,Zhang, Hongfu,&Schmitt, Axel K..(2014).U-series zircon age constraints on the plumbing system and magma residence times of the Changbai volcano, China/North Korea border.LITHOS,200,169-180. |
MLA | Zou, Haibo,et al."U-series zircon age constraints on the plumbing system and magma residence times of the Changbai volcano, China/North Korea border".LITHOS 200(2014):169-180. |
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