Pn tomography with Moho depth correction from eastern Europe to western China

doi:10.1002/2016JB013052

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

	Pn tomography with Moho depth correction from eastern Europe to western China
	Lu, Yan 1; Ni, Sidao 2,3; Chen, Ling 4,5; Chen, Qi-Fu 1
刊名	JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
	2017-02-01
卷号	122 期号:2 页码:1284-1301
ISSN号	2169-9313
DOI	10.1002/2016JB013052
文献子类	Article
英文摘要	We proposed a modified Pn velocity and anisotropy tomography method by considering the Moho depth variations using the Crust 1.0 model and obtained high-resolution images of the uppermost mantle Pn velocity and anisotropy structure from eastern Europe to western China. The tomography results indicate that the average Pn velocities are approximately 8.0 and 8.1 km/s under the western and eastern parts of the study area, respectively, with maximum velocity perturbations of 3%-4%. We observed high Pn velocities under the Adriatic Sea, Black Sea, Caspian Sea, Arabian Plate, Indian Plate, and in the Tarim and Sichuan Basins but low Pn velocities under the Apennine Peninsula, Dead Sea fault zone, Anatolia, Caucasus, Iranian Plateau, Hindu Kush, and in the Yunnan and Myanmar regions. Generally, regions with stable structures and low lithospheric temperatures exhibit high Pn velocities. Low Pn velocities provide evidence for the upwelling of hot material, which is associated with plate subduction and continental collision processes. Our Pn velocity and anisotropy imaging results indicate that the Adriatic microplate dives to the east and west, the hot material upwelling caused by subduction beneath the Tibetan Plateau is not as significant as that in the Caucasus and Myanmar regions, the lithosphere exhibits coupled rotational movement around the Eastern Himalayan syntaxes, and the areas to the north and south of 26 degrees N in the Yunnan region are affected by different geodynamic processes. Our newly captured images of the uppermost mantle velocity and anisotropy structure provide further information about continental collision processes and associated dynamic mechanisms.
WOS关键词	UPPER-MANTLE BENEATH ; POSITIONING SYSTEM MEASUREMENTS ; TURKISH-IRANIAN PLATEAU ; SEISMIC ANISOTROPY ; TIBETAN PLATEAU ; WAVE TOMOGRAPHY ; HINDU-KUSH ; CONTINENTAL COLLISION ; CRUSTAL DEFORMATION ; BREAK-OFF
WOS研究方向	Geochemistry & Geophysics
语种	英语
出版者	AMER GEOPHYSICAL UNION
WOS记录号	WOS:000396132200027
资助机构	Chinese Academy of Sciences(XDB03010800) ; Chinese Academy of Sciences(XDB03010800) ; Chinese Academy of Sciences(XDB03010800) ; Chinese Academy of Sciences(XDB03010800) ; National Natural Science Foundation of China(41674066 ; National Natural Science Foundation of China(41674066 ; National Natural Science Foundation of China(41674066 ; National Natural Science Foundation of China(41674066 ; 41461164003 ; 41461164003 ; 41461164003 ; 41461164003 ; 41304065 ; 41304065 ; 41304065 ; 41304065 ; 41225016) ; 41225016) ; 41225016) ; 41225016) ; Chinese Academy of Sciences(XDB03010800) ; Chinese Academy of Sciences(XDB03010800) ; Chinese Academy of Sciences(XDB03010800) ; Chinese Academy of Sciences(XDB03010800) ; National Natural Science Foundation of China(41674066 ; National Natural Science Foundation of China(41674066 ; National Natural Science Foundation of China(41674066 ; National Natural Science Foundation of China(41674066 ; 41461164003 ; 41461164003 ; 41461164003 ; 41461164003 ; 41304065 ; 41304065 ; 41304065 ; 41304065 ; 41225016) ; 41225016) ; 41225016) ; 41225016) ; Chinese Academy of Sciences(XDB03010800) ; Chinese Academy of Sciences(XDB03010800) ; Chinese Academy of Sciences(XDB03010800) ; Chinese Academy of Sciences(XDB03010800) ; National Natural Science Foundation of China(41674066 ; National Natural Science Foundation of China(41674066 ; National Natural Science Foundation of China(41674066 ; National Natural Science Foundation of China(41674066 ; 41461164003 ; 41461164003 ; 41461164003 ; 41461164003 ; 41304065 ; 41304065 ; 41304065 ; 41304065 ; 41225016) ; 41225016) ; 41225016) ; 41225016) ; Chinese Academy of Sciences(XDB03010800) ; Chinese Academy of Sciences(XDB03010800) ; Chinese Academy of Sciences(XDB03010800) ; Chinese Academy of Sciences(XDB03010800) ; National Natural Science Foundation of China(41674066 ; National Natural Science Foundation of China(41674066 ; National Natural Science Foundation of China(41674066 ; National Natural Science Foundation of China(41674066 ; 41461164003 ; 41461164003 ; 41461164003 ; 41461164003 ; 41304065 ; 41304065 ; 41304065 ; 41304065 ; 41225016) ; 41225016) ; 41225016) ; 41225016)
内容类型	期刊论文
源URL	[http://ir.iggcas.ac.cn/handle/132A11/53088]
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	Lu, Yan
作者单位	1.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Earth & Planetary Phys, Beijing, Peoples R China 2.Chinese Acad Sci, Inst Geodesy & Geophys, State Key Lab Geodesy & Earths Dynam, Wuhan, Peoples R China 3.Univ Sci & Technol China, Sch Earth & Space Sci, Hefei, Peoples R China 4.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing, Peoples R China 5.CAS Ctr Excellence Tibetan Plateau Earth Sci, Beijing, Peoples R China
推荐引用方式 GB/T 7714	Lu, Yan,Ni, Sidao,Chen, Ling,et al. Pn tomography with Moho depth correction from eastern Europe to western China[J]. JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH,2017,122(2):1284-1301.
APA	Lu, Yan,Ni, Sidao,Chen, Ling,&Chen, Qi-Fu.(2017).Pn tomography with Moho depth correction from eastern Europe to western China.JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH,122(2),1284-1301.
MLA	Lu, Yan,et al."Pn tomography with Moho depth correction from eastern Europe to western China".JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH 122.2(2017):1284-1301.