CAJ | 학술논문

给出了2003-2008年新疆74次M_s≥4.5地震的震源机制解.分析了该期间震源机制反映出的新疆区域应力场特征,并结合1990-2008年的地震活动图像和区域应力场进行了讨论.结果认为:1990-2003年与2004-2008年新疆M_s≥5地震活动空间分布图像存在较大的差异性;震源机制得到的主压应力P轴方位为NNW向,与新疆近SN向的背景应力场和作者前期给出的NNE向结果略有差异,反映出不同时期新疆大区域应力场的变化特点;中强地震震源机制主压应力P轴仰角的大小变化与新疆地震活动的强弱相关性明显.
급출료2003-2008년신강74차M_s≥4.5지진적진원궤제해.분석료해기간진원궤제반영출적신강구역응력장특정,병결합1990-2008년적지진활동도상화구역응력장진행료토론.결과인위:1990-2003년여2004-2008년신강M_s≥5지진활동공간분포도상존재교대적차이성;진원궤제득도적주압응력P축방위위NNW향,여신강근SN향적배경응력장화작자전기급출적NNE향결과략유차이,반영출불동시기신강대구역응력장적변화특점;중강지진진원궤제주압응력P축앙각적대소변화여신강지진활동적강약상관성명현.
The paper presents the focal mechanism solutions of 74 earthquakes with M_s=4. 5 from 2003 to 2008 in Xinjiang and analyzes the regional stress field characteristics reflected by these focal mechanism solutions in Xinjiang in this period. Then, discussion has been made combining with the seismicity image and regional stress field from 1990 to 2008. The result shows that,spatial seismic activity patterns of earthquakes with M_s=5 in Xinjiang are quite different between 1990-2003 and 2004-2008. The seismic activity of mid-strong earthquakes or larger from 1990 to 2003 concentrated in the Aletai seismic belt, the eastern Tianshan mountains and the Arjin-Kunlun mountains tectonic belt. During this period, there occurred respectively the M_s7. 3 Zaisang earthquake in June, 1990, the M_s7. 8 Mani earthquake in 1997 ,the M_s8. 1 west of Kunlun mountain pass earthquake in 2001and the M_s7. 9 earthquake in the border area between China,Russia and Mongolia in 2003. Since 2004,the seismic activity of mid-strong earthquakes showed a trend of decreasing towards west in Xinjiang. The azimuth of the principal compression stress P axis of focal mechanism solutions is NNW, which is slightly different from the background stress field of near SN and the earlier result of NNE obtained by the author. It reflects the changing characteristic of the large-scale regional stress field in different times in Xinjiang. The inversion result of three regional stress fields reveals some difference in space. The middle area of Tianshan mountains is obviously under the stress field of NNW direction; In the west of South Tianshan mountains-Wuqia and Hetian area and its surroundings, the principal compression stress has the characteristic of NE. The change of elevation angles of the principal compression stress P axis in the focal mechanism solutions of mid-strong earthquakes is obviously related with the strong and weak seismic activities in Xinjiang.