Crustal and Upper Mantle Structure Beneath the Southeastern United States From Joint Inversion of Receiver Functions and Rayleigh Wave Dispersion
文献类型:期刊论文
作者 | Yang, Qiuyue1; Liu, Kelly H.1; Wang, Tuo1,2; Song, Jianguo1,3; Gao, Stephen S.1 |
刊名 | JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
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出版日期 | 2021-10-01 |
卷号 | 126期号:10页码:18 |
关键词 | crustal structure receiver function Rayleigh wave dispersion mantle structure southeastern U S eclogitization |
ISSN号 | 2169-9313 |
DOI | 10.1029/2021JB021846 |
英文摘要 | Using data from 186 stations belonging to the USArray Transportable Array, a three-dimensional shear wave velocity model for the southeastern United States is constructed for the top 180 km by a joint inversion of receiver functions and Rayleigh wave phase velocity dispersion computed from ambient noise and teleseismic earthquake data. The resulting shear wave velocity model and the crustal thickness and Vp/Vs (kappa) measurements show a clear spatial correspondence with major surficial geological features. The distinct low velocities observed in the depth range of 0-25 km beneath the eastern Gulf Coastal Plain reflect the thick layer of unconsolidated or poorly consolidated sediments atop the crystalline crust. The low kappa (1.70-1.74) and slow lowermost crustal velocities observed beneath the eastern Southern Appalachian Mountains (including the Carolina Terrane and Inner Piedmont) relative to the adjacent Blue Ridge Mountains and Valley and Ridge can be interpreted by lower crustal delamination followed by relamination. The Osceola intrusive complex in the central Suwannee Terrane has similar crustal characteristics as the eastern Southern Appalachian Mountains and thus can similarly be attributed to crustal delamination/relamination processes. The Grenville Province and adjacent areas possess relatively high kappa values which can be attributed to mafic intrusion associated with crustal extension in a recently recognized segments of the eastern arm of the Proterozoic Midcontinent Rift. |
WOS关键词 | SEISMIC VELOCITY STRUCTURE ; LOWER CONTINENTAL-CRUST ; SOUTHERN APPALACHIANS ; AMBIENT NOISE ; SURFACE-WAVE ; TECTONIC DEVELOPMENT ; MIDCONTINENT RIFT ; SHALLOW MANTLE ; TERRANE ; REFLECTION |
资助项目 | American Chemical Society[PRF-60281-ND8] ; U.S. National Science Foundation[1919789] |
WOS研究方向 | Geochemistry & Geophysics |
语种 | 英语 |
WOS记录号 | WOS:000711968800008 |
出版者 | AMER GEOPHYSICAL UNION |
资助机构 | American Chemical Society ; American Chemical Society ; U.S. National Science Foundation ; U.S. National Science Foundation ; American Chemical Society ; American Chemical Society ; U.S. National Science Foundation ; U.S. National Science Foundation ; American Chemical Society ; American Chemical Society ; U.S. National Science Foundation ; U.S. National Science Foundation ; American Chemical Society ; American Chemical Society ; U.S. National Science Foundation ; U.S. National Science Foundation |
源URL | [http://ir.iggcas.ac.cn/handle/132A11/103773] ![]() |
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 | Gao, Stephen S. |
作者单位 | 1.Missouri Univ Sci & Technol, Geol & Geophys Program, Rolla, MO 65409 USA 2.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing, Peoples R China 3.China Univ Petr East China, Sch Geosci, Qingdao, Peoples R China |
推荐引用方式 GB/T 7714 | Yang, Qiuyue,Liu, Kelly H.,Wang, Tuo,et al. Crustal and Upper Mantle Structure Beneath the Southeastern United States From Joint Inversion of Receiver Functions and Rayleigh Wave Dispersion[J]. JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH,2021,126(10):18. |
APA | Yang, Qiuyue,Liu, Kelly H.,Wang, Tuo,Song, Jianguo,&Gao, Stephen S..(2021).Crustal and Upper Mantle Structure Beneath the Southeastern United States From Joint Inversion of Receiver Functions and Rayleigh Wave Dispersion.JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH,126(10),18. |
MLA | Yang, Qiuyue,et al."Crustal and Upper Mantle Structure Beneath the Southeastern United States From Joint Inversion of Receiver Functions and Rayleigh Wave Dispersion".JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH 126.10(2021):18. |
入库方式: OAI收割
来源:地质与地球物理研究所
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