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《Chinese Journal of Geophysics》 2005-01
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Tomographic imaging of 3-D crustal structure beneath Changbaishan—Tianchi volcano region

YANG Zhuo-Xin, ZHANG Xian-Kang, ZHAO Jin-Ren YANG Jian, DUAN Yu-Ling, WANG Shuai-Jun Center of Exploration Geophysics,China Earthquake Administration,Zhengzhou 450002,China  
Using reflection traveltimes of P wave from the 3-D spatial deep seismic sounding experiment carried out in the Changbai—Tianchi volcanic region, we have reconstructed 3-D crustal interfaces and crustal velocity distribution images by the seismic tomography technique. The interface images show that the crustal depth increases from NW to SE in general. The Ma'anshan—Sandaobaihe and Fu'erhe-Hongqihe faults are two main deep structures of this region, especially in both sides of Ma'anshan—Sandaobaihe fault, where the change of crustal thickness is obvious, implying there is a crustal thickness variation belt or deep crustal fault at this position. The velocity images show that an obvious low-velocity anomaly of P-wave exists around the Tianchi at the depth of 10 km. It becomes a low-velocity anomalous strip of nearly SN direction at the 15 km depth, which extends about 80~90km in NS direction and 30~40km in EW direction. With the increase of depth, the low-velocity anomalous strip is distributed on the west side of the Tianchi, but with a smaller scale, and it distributes more concentrated and presents higher perturbation. This change image of the P-wave velocity anomaly illustrates the spatial distribution state of the magma system under the Tianchi volcano to certain extent.
【Fund】: 中国地震局“九五”重点项目 (95 11 0 2 0 1)资助
【CateGory Index】: P315
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