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- W2365882364 abstract "Luxi uplift is the important extensional tectonics in the North China Craton.In order to analyse the characteristics of crustal structure beneath the Luxi uplift,We collected 102 seismic waveforms(MS6.0,epicenter distance between 30°~90°)which recorded by 28 seismic stations in the Luxi uplift and its surrounding areas from 2010 to 2013,and we obtained the crustal thickness and Poisson's ratio beneath each station from Tele-seismic receiver function study.The results showed that:the crustal thickness of Luxi uplift area is between 29.9~36.1km,the crustal thickness is the thinnest in the north,mainly changes in the north-south direction and increases toward-south;In contrast,Luxi uplift average Poisson's ratio of crustal in northern area of Luxi uplift is largest,and gradually decreasing to south.According to the chatacteristics of the crustal structure and Poisson's ratio beneath Luxi uplift area,We concluded that the characteristics of crustal structure of Luxi uplift area are caused by the mantle upwelling actively and the earth's crust is been thermal erosion,especially the northern area of the Luxi uplift.The formation of Luxi uplift is the response of the lithospheric thinning of the North China in crust,and showed the lithospheric thinning process of the North China exists significant thermal erosion in Mesozoic." @default.
- W2365882364 created "2016-06-24" @default.
- W2365882364 creator A5053841786 @default.
- W2365882364 date "2015-01-01" @default.
- W2365882364 modified "2023-09-28" @default.
- W2365882364 title "The crustal thickness and Poisson's ratio beneath the Luxi uplift area and its geological significance" @default.
- W2365882364 hasPublicationYear "2015" @default.
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