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- W2348584906 abstract "The travel time of natural earthquakes and the tomography of S-wave seismic phase can provide the fine images of S-wave velocity disturbance of the Upper Mantle.The study of the high-resolution S-wave tomography of the eastern part of North China(32°～44°N,115°～126°E)has revealed the velocity structure differences of the upper mantle between Su-Lu areas and circum-Bohai Bay areas;this result has yielded new geophysical evidences and constraints for the further research of the regional deep structure evolution.The remarkable achievement of this paper is the recognition of two Upper Mantle crack zones indicated by the dramatic variations of the seismic velocities,which occur separately under the Bohai Bay rift area and the Su-Lu ultrahigh pressure metamorphic belt.The crack zone under the Su-Lu ultrahigh pressure metamorphic belt embraces multiple sequentially arranged high velocity blocks,which are supposed to be genetically connected with(1)the strike-slip faulting and the forward subduction of the Yangtze plate,and(2)the subduction and exhumation mechanism of the frontier ultrahigh pressure metamorphic blocks.The results of the Upper Mantle S-wave seismic velocity tomography support that an Upper Mantle plume system has been developing in the Bohai Bay areas;these results also offer a new criterion for distinguishing the plume system." @default.
- W2348584906 created "2016-06-24" @default.
- W2348584906 creator A5032345488 @default.
- W2348584906 date "2007-01-01" @default.
- W2348584906 modified "2023-09-23" @default.
- W2348584906 title "Upper Mantle Crack Zones in the Eastern Part of North China" @default.
- W2348584906 hasPublicationYear "2007" @default.
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