Crustal structure beneath Northeast China from ambient noise tomography

doi:10.1016/j.pepi.2019.04.008

CORC > 地质与地球物理研究所 > 中国科学院地质与地球物理研究所 > 中国科学院地球与行星物理重点实验室

	Crustal structure beneath Northeast China from ambient noise tomography
	Yang, Yu 1,2; Lei, Jianshe 2; Ai, Yinshuang 3; Zhang, Guangwei 2; Sun, Changqing 2; Fan, Enbo 3; Li, Long 3; Mi, Qi 2; Lu, Mingwen 2; He, Jing 2
刊名	PHYSICS OF THE EARTH AND PLANETARY INTERIORS
	2019-08-01
卷号	293 页码:18
关键词	Intraplate volcanism Crustal structure Ambient noise tomography Northeast China
ISSN号	0031-9201
DOI	10.1016/j.pepi.2019.04.008
英文摘要	To investigate the deep origin of Cenozoic intraplate volcanism in Northeast (NE) China, especially the Wudalianchi volcanism, a new 3-D S-wave velocity model of the crust and uppermost mantle is constructed through ambient noise tomography. Rayleigh wave phase velocity dispersion curves of 5-40 s periods are collected from seismograms recorded at our newly deployed WAVESArray portable stations around the Wudalianchi volcano and NECESSArray portable stations and CEA provincial seismic stations in NE China. Compared to images resolved in previous studies, the addition of WAVESArray data provides much higher resolution in NE China. Under the Songliao, Erlian and Hailar basins, obvious low-velocity (low-V) anomalies are imaged above 5 km depth, which are well correlated with the sediments and have good correlations with the outlines of the basins. Under the Changbaishan volcano and Abaga and Halaha volcanic groups, low-V anomalies extend continuously down to the uppermost mantle, suggesting their continuous mantle magma provision. Under the Wudalianchi volcano, low-V anomalies above 20 km depth and in the upper mantle are revealed, but a high-velocity anomaly zone appears in the lower crust, suggesting that the Wudalianchi volcano is a type of mantle origin but parts of magma have been solidified in the lower crust, likely due to intermittent mantle magma provision. All these results indicate that the intraplate volcanism in NE China could be related to complicated mantle dynamics of the big mantle wedge that has been formed due to the stagnancy and dehydration of the subducted Pacific slab in the mantle transition zone.
资助项目	National Natural Science Foundation of China (NSFC)[41530212] ; National Natural Science Foundation of China (NSFC)[41674091] ; National Natural Science Foundation of China (NSFC)[41474040] ; ICD Basic Scientific Study Special Grant[ZDJ2015-17] ; Strategic Priority Research Program (B) of Chinese Academy of Sciences[XDB18000000] ; DREAM Project of MOST, China[2016YFC0600408] ; 10,000 Talents Award from the Chinese government
WOS关键词	WAVE VELOCITY STRUCTURE ; MANTLE TRANSITION ZONE ; NE CHINA ; INTRAPLATE VOLCANISM ; NEIGHBORHOOD ALGORITHM ; GEOPHYSICAL INVERSION ; HEILONGJIANG PROVINCE ; EASTERN HEILONGJIANG ; PERIDOTITE XENOLITHS ; LITHOSPHERIC MANTLE
WOS研究方向	Geochemistry & Geophysics
语种	英语
出版者	ELSEVIER
WOS记录号	WOS:000479018800003
资助机构	National Natural Science Foundation of China (NSFC) ; National Natural Science Foundation of China (NSFC) ; ICD Basic Scientific Study Special Grant ; ICD Basic Scientific Study Special Grant ; Strategic Priority Research Program (B) of Chinese Academy of Sciences ; Strategic Priority Research Program (B) of Chinese Academy of Sciences ; DREAM Project of MOST, China ; DREAM Project of MOST, China ; 10,000 Talents Award from the Chinese government ; 10,000 Talents Award from the Chinese government ; National Natural Science Foundation of China (NSFC) ; National Natural Science Foundation of China (NSFC) ; ICD Basic Scientific Study Special Grant ; ICD Basic Scientific Study Special Grant ; Strategic Priority Research Program (B) of Chinese Academy of Sciences ; Strategic Priority Research Program (B) of Chinese Academy of Sciences ; DREAM Project of MOST, China ; DREAM Project of MOST, China ; 10,000 Talents Award from the Chinese government ; 10,000 Talents Award from the Chinese government ; National Natural Science Foundation of China (NSFC) ; National Natural Science Foundation of China (NSFC) ; ICD Basic Scientific Study Special Grant ; ICD Basic Scientific Study Special Grant ; Strategic Priority Research Program (B) of Chinese Academy of Sciences ; Strategic Priority Research Program (B) of Chinese Academy of Sciences ; DREAM Project of MOST, China ; DREAM Project of MOST, China ; 10,000 Talents Award from the Chinese government ; 10,000 Talents Award from the Chinese government ; National Natural Science Foundation of China (NSFC) ; National Natural Science Foundation of China (NSFC) ; ICD Basic Scientific Study Special Grant ; ICD Basic Scientific Study Special Grant ; Strategic Priority Research Program (B) of Chinese Academy of Sciences ; Strategic Priority Research Program (B) of Chinese Academy of Sciences ; DREAM Project of MOST, China ; DREAM Project of MOST, China ; 10,000 Talents Award from the Chinese government ; 10,000 Talents Award from the Chinese government
内容类型	期刊论文
源URL	[http://ir.iggcas.ac.cn/handle/132A11/93349]
专题	地质与地球物理研究所_中国科学院地球与行星物理重点实验室
通讯作者	Lei, Jianshe
作者单位	1.China Earthquake Adm, Inst Geophys, Beijing 100081, Peoples R China 2.China Earthquake Adm, Inst Crustal Dynam, Key Lab Crustal Dynam, Beijing 100085, Peoples R China 3.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Earth & Planetary Phys, Beijing 100029, Peoples R China
推荐引用方式 GB/T 7714	Yang, Yu,Lei, Jianshe,Ai, Yinshuang,et al. Crustal structure beneath Northeast China from ambient noise tomography[J]. PHYSICS OF THE EARTH AND PLANETARY INTERIORS,2019,293:18.
APA	Yang, Yu.,Lei, Jianshe.,Ai, Yinshuang.,Zhang, Guangwei.,Sun, Changqing.,...&Liu, Zemin.(2019).Crustal structure beneath Northeast China from ambient noise tomography.PHYSICS OF THE EARTH AND PLANETARY INTERIORS,293,18.
MLA	Yang, Yu,et al."Crustal structure beneath Northeast China from ambient noise tomography".PHYSICS OF THE EARTH AND PLANETARY INTERIORS 293(2019):18.