首页> 外文期刊>Journal of geophysical research. Solid earth: JGR >Insight into the origin of the Tengchong intraplate volcano and seismotectonics in southwest China from local and teleseismic data
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Insight into the origin of the Tengchong intraplate volcano and seismotectonics in southwest China from local and teleseismic data

机译:从本地和远震数据中了解中国西南部腾冲板内火山和地震构造的起源

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A high-resolution tomographic image of the crust and upper mantle under Yunnan Province in southwest China was determined by using a large number of teleseismic data measured precisely from digital seismograms as well as local- earthquake arrival times recorded by the dense Yunnan seismic network. The grid spacing of the tomographic model is —70 km x 78 km in the horizontal directions and 4-70 km in depth. Our resulting model shows a clear low-velocity (low-V, <-0.3% with respect to the average one-dimensional velocity model) column extending from the surface down to about 400-km depth under the active Tengchong volcano and some high-velocity (high-V) anomalies existing in the mantle transition zone. Furthermore, the low-V anomaly extends horizontally toward the northeast at —250- to 400-km depth. Combining our tomographic results with geochemical and geological investigations, we infer that the Tengchong volcano is a rift-related volcano caused by the subduction and dehydration of the Indian plate as well as corner flow in the mantle wedge, though the subducted slab is a continental plate. Our results show that the upwelling flow under Tengchong originates at —400-km depth. A prominent low-V anomaly along the Red River fault zone extends down to the upper mantle (-100-km depth), reflecting that the Red River fault zone may have cut through the crust to the upper mantle. The two Dayao earthquakes (M 6.1 and M 6.2) in 2003 occurred on the margin of high-V anomalies and are underlain by a prominent low-V anomaly in the lower crust and upper mantle, suggesting that the Dayao earthquakes may be associated with fluids released from the dehydration of the subducted Indian slab. These results are significantly improved compared with previous studies and provide new seismic constraints on the dynamic processes of the India-Asia collision.
机译:通过使用大量从数字地震图精确测量的远震数据以及密集的云南地震台网记录的局部地震到达时间,来确定中国西南部云南省地壳和上地幔的高分辨率层析图像。层析成像模型的网格间距在水平方向上为70 km x 78 km,在深度方向上为4-70 km。我们得到的模型显示出清晰的低速(低V,相对于平均一维速度模型,-V小于-0.3%)柱从活动的腾冲火山和一些高强度火山下的地表向下延伸至约400公里的深度。地幔过渡带中存在的速度(高V)异常。此外,低伏异常在水平方向从250到400公里向东北水平延伸。将层析成像结果与地球化学和地质调查相结合,我们可以推断,腾冲火山是与裂谷有关的火山,是由印度板块的俯冲和脱水以及地幔楔的角流引起的,尽管俯冲板块是大陆板块。我们的结果表明,腾冲下的上升流起源于—400公里深度。沿红河断层带的一个显着的低伏异常向下延伸至上地幔(深度为100公里),这反映出红河断层带可能已经切穿了地壳并到达上地幔。 2003年的大姚地震两次(M 6.1和M 6.2)发生在高V异常的边缘,并且在下地壳和上地幔的一个显着的低V异常的基础上,这表明大姚地震可能与流体有关。从俯冲的印度板块的脱水中释放出来。与以前的研究相比,这些结果得到了显着改善,并为印度-亚洲碰撞的动力学过程提供了新的地震约束。

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