摘要
阿尔金断裂带作为青藏高原北部边界 ,其走滑量和走滑速率一直为地学界所关注 ,对这样一条大陆内部巨型走滑断裂带的滑动速率进行研究 ,对于了解阿尔金断裂带左旋走滑和青藏高原北部隆升之间的耦合关系 ,具有重要意义。在阿尔金断裂带东段的疏勒河口以西 ,阿尔金断裂错断了几条规模相近的河流阶地和洪积扇 ,形成典型的走滑断层断错地貌。通过对这些典型断错地貌点的地貌观测和年代学研究 ,得到阿尔金断裂带东段石堡城以东疏勒河以西自 2 0kaBP以来的滑动速率约为 4～ 5mm/a。自 50kaBP以来 ,阿尔金断裂带东段断层平均滑动速率具有较高的时间、空间一致性 ,约为 4～ 6mm/a ,表明利用河流阶地和洪积扇位错作为断层走滑位移标志计算断层滑动速率 ,具有较高的可信度。
As northern boundary of the Tibet Plateau, the Altyn Tagh Fault attracts the attention of lots of geo scientists from different parts of the world. The offset and slip rate of the Altyn Tagh Fault are a topic full of disputation. To make clear the slip rate of the Altyn Tagh Fault is important for understanding the coupling relationship between the uplift and strike slip on the northern Tibet Plateau. On the eastern Altyn Tagh Fault, to the west of the outlet of the Shulehe River, the late Quaternary terraces and alluvial fans are offset by the fault. There are some typical offset landforms in this region, and by investigating these geomorphological features, slip rate of the Altyn Tagh Fault can be evaluated. To the West of Shulehe River, three sites, Erjiatai, Niuyagou gully and Bagexia were surveyed for obtaining the slip rate on this part of the Altyn Tagh Fault. The range of fieldwork region for this study is about from 94°24′E to 94°37′E. At Erjiatai, offset of the lowest terrace T 1 cannot be identified because of its absence near the fault. The offsets of T 2, T 3 and T 4 terraces are 40m, 100m and 220m, respectively, and the TL ages of T 1, T 2 and T 3 terraces are 7.82ka BP, 22.53ka BP and 53 26ka BP. According to these data, we can calculate the average slip rates of the fault in different periods since late Quaternary. The slip rate of the fault at this site is about 4～4 5mm/yr since 50ka BP. At Niuyagou, the fault offset all the terraces but T 1. The offsets of T 2, T 3 and T 4 terraces are 6 4m, 40m and 120m, respectively, and the TL ages of T 1, T 2 and T 3 terraces are 6 97ka BP, 10 06ka BP and 28 81ka BP. So the slip rate of the fault here is about 4～4 2mm/yr since 30ka BP. At Bagexia, the lowest terrace T 1 is not offset by the fault but the other terraces above T 1 are offset by the fault. Here the slip rate of the fault is a little higher than the other two sites described above. Here the slip rate of the fault since 20ka BP is about 4 7mm/yr. Based on the above mentioned data the following conclusion can be drawn: The slip rate of the eastern Altyn Tagh Fault to the west of Shulehe River since 20ka BP is about 4～5mm/yr and the slip rate become a little higher westward. Regarding the strike of the Altyn Tagh Fault in this region is about N73°E, we may estimate that the strike slip on the eastern Altyn Tagh Fault assimilates the north south shortening of the Tibetan Plateau at a rate of 1 5mm/yr at maximum.
出处
《地震地质》
EI
CSCD
北大核心
2003年第3期349-358,共10页
Seismology and Geology
基金
地震科学联合基金 ( 1980 6 2 )
科技部项目 ( 95110 2 )中国地震局地球物理勘探中心论著编号RECG2 0 0 2 0 1
