根据昆明电信传输台网1983—1989年记录的区域地震初至 P 波走时资料,用参数分离和多事件定位的方法得到台网内各台站的 P 波走时校正值.这组校正值在一定程度上反映了该地区地壳上部横向不均匀结构的特征.台站校正值的地理分布明显地分...根据昆明电信传输台网1983—1989年记录的区域地震初至 P 波走时资料,用参数分离和多事件定位的方法得到台网内各台站的 P 波走时校正值.这组校正值在一定程度上反映了该地区地壳上部横向不均匀结构的特征.台站校正值的地理分布明显地分为3个地区:台站最密集的滇西地区,所有台站(不包括南边的云县,施甸和畹町)的台站校正值不超过0.15s;东部地区(楚雄以东)台站分布仍较密集,但间距比滇西大,其中大部分台站显示为正延迟;南部地区包括文山、思茅、普洱以及云县、施甸和畹町,它们均显示出较大的负延迟.这与云南地区的地质构造特征基本上是一致的.走时校正后重新定位的精度有较大的提高,因此,这组台站校正值可以提供地震台网的常规定位使用.展开更多
Based on the P wave first arrival time data of 275 local earthquakes recorded by Kunming Telemetered Seismic Network from 1982 to 1989, a 3-D velocity structure beneath the network was obtained by the separationmethod...Based on the P wave first arrival time data of 275 local earthquakes recorded by Kunming Telemetered Seismic Network from 1982 to 1989, a 3-D velocity structure beneath the network was obtained by the separationmethod of focal parameter and medium structure parameter and 3-D approximate ray tracing. In view of 'thesituation that the intervals between stations in the network is relatively long, and the local first arrival phasemay be Pn instead of P, so we simulated Pn as the diving wave from the layer beneath Moho and using approximate ray tracing method on the grid model. The final 3-D velocity structure is basically consistent withthe result from the deep seismic sounding and the anomaly inversion of Bouguer gravity. The Dianzhong area(in the vicinity of Dukou and Chuxiong) shows an obvious high velocity zone at depth of 45 km, which canbe interpreted as the uplift of Moho discontinuity. The upper crust in this area displays lower velocity zone,so the uplift of Moho discontinuity is considered as the result of isostatic compensation. The configuration ofvelocity contours indicates that the upper crust and lower crust are complicated, while the middle crust is relatively simple. This feature reveals that Yunnan area belongs to modern tectonically active region. As themain boundary of the major tectonic units in the study area, although there is no obvious evidence about lowvelocity anomaly zone along the Red River Fault, the fault shows up th feature of sturctural divide on themid-lower crustal velocity contours, and it is inferred that the fault passes through the Moho-discontinuity atleast.展开更多
文摘根据昆明电信传输台网1983—1989年记录的区域地震初至 P 波走时资料,用参数分离和多事件定位的方法得到台网内各台站的 P 波走时校正值.这组校正值在一定程度上反映了该地区地壳上部横向不均匀结构的特征.台站校正值的地理分布明显地分为3个地区:台站最密集的滇西地区,所有台站(不包括南边的云县,施甸和畹町)的台站校正值不超过0.15s;东部地区(楚雄以东)台站分布仍较密集,但间距比滇西大,其中大部分台站显示为正延迟;南部地区包括文山、思茅、普洱以及云县、施甸和畹町,它们均显示出较大的负延迟.这与云南地区的地质构造特征基本上是一致的.走时校正后重新定位的精度有较大的提高,因此,这组台站校正值可以提供地震台网的常规定位使用.
文摘Based on the P wave first arrival time data of 275 local earthquakes recorded by Kunming Telemetered Seismic Network from 1982 to 1989, a 3-D velocity structure beneath the network was obtained by the separationmethod of focal parameter and medium structure parameter and 3-D approximate ray tracing. In view of 'thesituation that the intervals between stations in the network is relatively long, and the local first arrival phasemay be Pn instead of P, so we simulated Pn as the diving wave from the layer beneath Moho and using approximate ray tracing method on the grid model. The final 3-D velocity structure is basically consistent withthe result from the deep seismic sounding and the anomaly inversion of Bouguer gravity. The Dianzhong area(in the vicinity of Dukou and Chuxiong) shows an obvious high velocity zone at depth of 45 km, which canbe interpreted as the uplift of Moho discontinuity. The upper crust in this area displays lower velocity zone,so the uplift of Moho discontinuity is considered as the result of isostatic compensation. The configuration ofvelocity contours indicates that the upper crust and lower crust are complicated, while the middle crust is relatively simple. This feature reveals that Yunnan area belongs to modern tectonically active region. As themain boundary of the major tectonic units in the study area, although there is no obvious evidence about lowvelocity anomaly zone along the Red River Fault, the fault shows up th feature of sturctural divide on themid-lower crustal velocity contours, and it is inferred that the fault passes through the Moho-discontinuity atleast.
