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《Chinese Journal of Geophysics》 2014-01
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A traveltime tomography study by teleseismic S wave data in the Northeast China area

ZHANG Feng-Xue;WU Qing-Ju;LI Yong-Hua;Key Laboratory of Seismic Observation and Geophysical Imaging,Institute of Geophysics, China Earthquake Administration;Institute of Geophysics,China Earthquake Administration1Beijing 100081,China;Institute of Geophysics,China Earthquake Administration;  
We picked 10301Swave relative traveltime residuals from the teleseismic waveform data by waveform correlation method.The teleseismic waveform data were recorded by the temporary and permanent seismic networks in Northeast China from June 2009to May 2011,the total number of the station is 234.We imaged the S-wave velocity structure beneath Northeast China down to 800km depth by two ray traveltime tomography methods.The S-wave velocity anomaly structures are partly restricted by the two different tomography results in this area.Most parts of the S wave results are similar to the previous P wave results:There is a high-velocity anomaly beneath the Changbaishan volcano,maybe this anomaly is the Pacific Plate,which subducted under the Eurasian Plate.Because of the local depressing of the plate,the shape of the plate doesn′t appear as an obvious slab.There are low-velocity anomalies beneath the Changbaishan volcano,A′ershan volcano and Wudalianchi volcano.The low-velocity anomalies under the Changbaishan and A′ershan volcano extend down to the near area of mantle transition zone,while the low-velocity anomaly under the Wudalianchi volcano extends down to about 200km depth,which may indicate that Changbaishan and A′ershan volcano have some relationship with the low-velocity anomalies under them,and the different depths of the low-velocity anomalies represent the different origin of the Wudalianchi volcano.There is a mainly highvelocity zone with a mixture high-and low-velocity distribution character beneath the Songliao Basin area.The mixture character suggests that the lithospheric mantle may have suffered destruction and transformation,and lithospheric delamination may have occurred and greatly affected the Songliao Basin.The low-velocity anomaly beneath the southern part of Songliao Basin area is connected to the low-velocity anomalies beneath the Changbaishan and A′ershan volcano,which may be a upwelling material channel from the lower mantle.We show the upper mantle S wave anomaly structure of Northeast China,which is similar to the P wave result but from another perspective,and provides an important constraint on our understanding of this area.
【Fund】: 国家自然科学基金重点项目(90814013);国家自然科学基金(41304066)联合资助;; 国土资源部深部探测技术实验研究专项(SinoProbe-02-03);; 中国地质调查局地质调查工作项目(1212011121072)
【CateGory Index】: P315.2
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