中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Mid-lithosphere discontinuities beneath the western and central North China Craton

文献类型:期刊论文

作者Sun, Weijia1; Kennett, B. L. N.2
刊名GEOPHYSICAL RESEARCH LETTERS
出版日期2017-02-16
卷号44期号:3页码:1302-1310
ISSN号0094-8276
DOI10.1002/2016GL071840
文献子类Article
英文摘要By analyzing P reflectivity extracted from stacked autocorrelograms for teleseismic events on a dense seismic profile, we obtain a detailed image of the mid-lithosphere discontinuity (MLD) beneath western and central North China Craton (NCC). This seismic daylight imaging exploits a broad high-frequency band (0.5-4 Hz) to reveal the fine-scale component of multi-scale lithospheric heterogeneity. The depth of the MLD beneath the western and central parts of the NCC ranges 80-120 km, with a good match to the transition to negative S velocity gradient with depth from Rayleigh wave tomography. The MLD inferred from seismic daylight imaging also has good correspondence with the transition from conductive to convective regimes estimated from heat flow data indicating likely thermal control within the seismological lithosphere.
WOS关键词UPPER-MANTLE ; TECTONIC EVOLUTION ; MOHO DEPTH ; DESTRUCTION ; CONSTRAINTS ; CRUSTAL ; MAP ; AUTOCORRELOGRAMS ; HETEROGENEITY ; AUSTRALIA
WOS研究方向Geology
语种英语
WOS记录号WOS:000396115000014
出版者AMER GEOPHYSICAL UNION
资助机构National Natural Science Foundation of China(41630210 ; National Natural Science Foundation of China(41630210 ; State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences ; State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences ; Youth Innovation Promotion Association CAS(2017094) ; Youth Innovation Promotion Association CAS(2017094) ; 41474105) ; 41474105) ; National Natural Science Foundation of China(41630210 ; National Natural Science Foundation of China(41630210 ; State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences ; State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences ; Youth Innovation Promotion Association CAS(2017094) ; Youth Innovation Promotion Association CAS(2017094) ; 41474105) ; 41474105) ; National Natural Science Foundation of China(41630210 ; National Natural Science Foundation of China(41630210 ; State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences ; State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences ; Youth Innovation Promotion Association CAS(2017094) ; Youth Innovation Promotion Association CAS(2017094) ; 41474105) ; 41474105) ; National Natural Science Foundation of China(41630210 ; National Natural Science Foundation of China(41630210 ; State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences ; State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences ; Youth Innovation Promotion Association CAS(2017094) ; Youth Innovation Promotion Association CAS(2017094) ; 41474105) ; 41474105)
源URL[http://ir.iggcas.ac.cn/handle/132A11/53095]  
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Sun, Weijia
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Earth & Planetary Phys, Beijing, Peoples R China
2.Australian Natl Univ, Res Sch Earth Sci, Canberra, ACT, Australia
推荐引用方式
GB/T 7714
Sun, Weijia,Kennett, B. L. N.. Mid-lithosphere discontinuities beneath the western and central North China Craton[J]. GEOPHYSICAL RESEARCH LETTERS,2017,44(3):1302-1310.
APA Sun, Weijia,&Kennett, B. L. N..(2017).Mid-lithosphere discontinuities beneath the western and central North China Craton.GEOPHYSICAL RESEARCH LETTERS,44(3),1302-1310.
MLA Sun, Weijia,et al."Mid-lithosphere discontinuities beneath the western and central North China Craton".GEOPHYSICAL RESEARCH LETTERS 44.3(2017):1302-1310.

入库方式: OAI收割

来源:地质与地球物理研究所

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