中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Analysis of H-kappa stacking of receiver functions beneath crust with complex structure: taking the Anatolia Plate as an example

文献类型:期刊论文

作者Wei Zi-Gen1; Chu Ri-Sheng1; Chen Ling2,3; Chong Jia-Jun1; Li Zhi-Wei1
刊名CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION
出版日期2016-11-01
卷号59期号:11页码:4048-4062
关键词H-kappa stacking of receiver functions Waveform inversion Sediment Crust-mantle transition zone Anatolia plate
DOI10.6038/cjg20161110
文献子类Article
英文摘要We calculated the synthetic receiver functions and their H-kappa stacking results for crust with different sediments and crust-mantle transition zones, and then inverted the crustal thickness (H) and V-p/V-s ratio (kappa) and S-wave velocity beneath the Anatolia plate with complex tectonic evolution history by H-kappa stacking and waveform inversion of receiver functions. The synthetic tests show: H-kappa stacking method is invalid in cases of existence of thick sediment or coexistence of sediment and crust-mantle transition zone; H obtained by H-kappa stacking is located in the transition zone and close to the top of transition zone with the increase of frequency in gradual crust-mantle transition zone; multiple extreme values exist in the H-kappa stacking and the last result is probably related to the crustal structure above the biggest wave impedance interface for inverted crust -mantle transition zone; the change of 1 km . s(-1) of P velocity results in 7 km variation of H but has little impact on kappa. The real data analysis show: prominent lateral inhomogeneity in H and k and S-wave velocity were observed beneath the north Anatolian plate, with sediment of <0. 5 km thick in most of the region and >3 km thick crust -mantle transition zone in local area; the north Anatolia fault extends to the mantle with existence of fluid in local area; residual old blocks may exist in the crust of the study region. Based on this study, we propose that the careful analysis of the waveform and changing trend along the azimuth of the receiver functions and the combination with other seismic methods can help to obtain reliable structural information for crust with complex structure by the H-kappa stacking method.
WOS关键词NORTH CHINA CRATON ; MOHO DEPTH ; TECTONIC IMPLICATIONS ; REGIONAL DIFFERENCES ; POISSONS RATIO ; ANISOTROPY ; THICKNESS ; TURKEY ; EVOLUTION ; FAULT
WOS研究方向Geochemistry & Geophysics
语种英语
WOS记录号WOS:000387300200010
源URL[http://ir.iggcas.ac.cn/handle/132A11/53268]  
专题地质与地球物理研究所_岩石圈演化国家重点实验室
作者单位1.Inst Geodesy & Geophys, State Key Lab Geodesy & Earths Dynam, Wuhan 430077, Peoples R China
2.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
3.Chinese Acad Sci, Ctr Excellence Tibetan Plateau Earth Sci, Beijing 100101, Peoples R China
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Wei Zi-Gen,Chu Ri-Sheng,Chen Ling,et al. Analysis of H-kappa stacking of receiver functions beneath crust with complex structure: taking the Anatolia Plate as an example[J]. CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION,2016,59(11):4048-4062.
APA Wei Zi-Gen,Chu Ri-Sheng,Chen Ling,Chong Jia-Jun,&Li Zhi-Wei.(2016).Analysis of H-kappa stacking of receiver functions beneath crust with complex structure: taking the Anatolia Plate as an example.CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION,59(11),4048-4062.
MLA Wei Zi-Gen,et al."Analysis of H-kappa stacking of receiver functions beneath crust with complex structure: taking the Anatolia Plate as an example".CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION 59.11(2016):4048-4062.

入库方式: OAI收割

来源:地质与地球物理研究所

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