Surface Rupture Features of the Akto MS 6.7 Earthquake in 2016 and Modern Tectonic Stress Field of Pamir
-
摘要: 帕米尔高原位于地中海－喜马拉雅地震带上，晚新生代以来随着印度板块向欧亚板块持续不断地挤压汇聚，其构造运动是欧亚大陆最强烈的地区。高原腹地发育一系列近SN向正断层，包括近SN向的塔什库尔干正断层所处的帕米尔中部现代区域的构造应力场以EW向水平拉张为主。2016年11月25日发生的阿克陶MS 6.7级地震的发震构造为塔什库尔干断层分支的NWW向木吉盆地北缘断层，其具有右旋走滑兼正断性质。地震在震中附近产生同震地表形变带，全长约1km，呈近SN－NNE向水平拉伸，发育近EW—NWW向的张裂缝，为地震破裂的产物，张裂缝的最大水平拉伸位移量和最大垂直位移量分别为46cm和16cm。地表破裂带中的NE和NW向张剪裂缝只是连接贯通这些雁列的张裂缝，其水平相对位移量取决于张裂缝的水平拉伸量和张裂缝之间的几何关系。地表形变带表现的拉张性质与帕米尔高原腹地区域现代应力场最大主压应力为垂直向基本一致，可能与深部热物质上涌造成的上地壳拉伸有关。而地表形变带呈近SN向水平拉张，与区域近EW向拉张应力场之间存在显著差异，这可能是木吉盆地北缘右旋走滑正断层阶区局部应力场调整的结果。Abstract: The Pamir plateau is located in the Mediterranean-Himalayan seismic zones. In late Cenozoic as Indian plate has continuously subducted with the Eurasian plate, its tectonic movement become the strongest in the Eurasian continent. In the interior of the plateau where are series of near S-N-striking normal faults, including near S-N-striking Taxkorgan fault, the modern tectonic stress field in central Pamir suggests mainly E-W directed extension. The seismogenic structure is the N-W-W-striking northern margin of the Muji basin fault, a branch of the Tashkurgan fault, which is the dextral strike-slip and normal active fault. The coseismic surface deformation zone produced by the Akto MS 6.7 earthquake is about 1km long, along EW-NWW trending. The horizontally tectonic movement is EW-NWW trending tensile fractures, which are the main earthquake ruptures. The maximum horizontal displacement is 46cm and the maximum vertical displacement is 16cm. The NE and NW trending shear cracks in the surface rupture zone are only connected to these fissures, and the horizontal relative displacement depends on the geometric relationship of the tensile fractures and horizontal tensile displacement. Extension properties of the surface deformation with maximum vertical principal stress are about in consistent with regional stress in the interior of the Pamir plateau, in which related upwelling hot material may result in the upper crust extending. The surface deformation zone has near S-N directed horizontal extension. Compared with near E-W directed extension in the region stress field, the difference is significant, which may be interpreted to adjust the partial stress field of the step between two dextral strike-slip and normal faults of the northern margin of the Muji basin faults.
-
Key words:
- Akto earthquake /
- Surface rupture zone /
- Tensile stress /
- Taxkorgan fault /
- Pamir
-
图 1 阿克陶地震地表破裂带展布
1.木吉盆地北缘断层；2.地表破裂带；3.微观震中；4.破裂分段
Figure 1. Distribution of the surface ruptures of the Akto earthquake
图 2 地表破裂带西段几何分布
Figure 2. The geometric distribution in the western segment of the surface rupture zone
图 3 地表破裂带中段地裂缝穿过居民点造成土木结构房屋倒塌
Figure 3. Collapse of civil structures caused by ground ruptures in the middle segment of surface rupture through the residential area
图 4 地表破裂带东段地裂缝水平和垂直拉张位移量
Figure 4. Horizontal and vertical tensile displacements in the east segment of surface rupture
图 5 地表破裂带张裂缝与张剪裂缝简化几何关系
Figure 5. Simplified geometric relationship between tensile and shear cracks in surface rupture zone
图 6 帕米尔高原主要活动断层分布图
（1）塔拉斯—费尔干纳右旋走滑断层；（2）吐尔尕特逆断层；（3）迈丹逆断层；（4）柯坪逆断层；（5）塔里木北缘逆断层；（6）卡兹克阿尔特逆断层；（7）阿赖山山前逆断层；（8）塔什库尔干正断层；（9）朗库里正断层；（10）穆尔加布正断层；（11）喀拉库尔正断层；（12）克孜勒陶－库斯拉普右旋走滑逆断层；（13）康西瓦左旋走滑断层；（14）喀喇昆仑－狮泉河右旋走滑断层；（15）喜马拉雅主中央逆断层；（16）喜马拉雅主边界逆断层；（17）旁遮普逆断层；（18）基尔达－苏来曼左旋走滑断层；（19）查曼左旋走滑断层；（20）贾拉拉巴德－瓦罕左旋走滑断层；（21）赫拉特右旋走滑断层；（22）巴格兰右旋走滑断层；（23）加巴什左旋走滑断层；（24）塔维尔达拉左旋走滑断层；（25）瓦赫什左旋走滑逆断层；（26）苏杨博斯－萨哈图孜逆断层；（27）图尔孙扎德－赛拉布逆断层；（28）纳伦盆地南缘逆断层；（29）加兹利右旋逆断层
Figure 6. Distribution of the main active faults of Pamir plateau
-
陈杰, 李涛, 李文巧等, 2011.帕米尔构造结及邻区的晚新生代构造与现今变形.地震地质, 33(2):241-259. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=dzdz201102006&dbname=CJFD&dbcode=CJFQ 李文巧, 2014.帕米尔高原东北部塔什库尔干谷地活动构造与强震.国际地震动态, (8):35-41. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=gjzt201408007&dbname=CJFD&dbcode=CJFQ 马杏垣, 1989.中国岩石圈动力学地图集.北京:中国地图出版社. 宁杰远, 臧绍先, 1990.帕米尔-兴都库什地区地震空间分布特征及应力场特征.地球物理学报, 33(6):657-669. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=dqwx199006004&dbname=CJFD&dbcode=CJFQ 宋扬, 胡建中, 王瑞江等, 2011.帕米尔弧东段逆冲推覆构造特征.现代地质, 25(1):15-21. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=xddz201101002&dbname=CJFD&dbcode=CJFQ 伍秀芳, 刘胜, 汪新等, 2004.帕米尔-西昆仑北麓新生代前陆褶皱冲断带构造剖面分析.地质科学, 39(2):260-271. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=dzkx200402012&dbname=CJFD&dbcode=CJFQ 田勤俭, 丁国瑜, 郝平等, 2006.南天山及塔里木北缘构造带西段地震构造研究.地震地质, 28(2):213-223. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=dzdz200602004&dbname=CJFD&dbcode=CJFQ 徐锡伟, 谭锡斌, 吴国栋等, 2011.2008年于田MS 7.3地震地表破裂带特征及其构造属性讨论.地震地质, 33(2):462-471. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=dzdz201102024&dbname=CJFD&dbcode=CJFQ 张浪平, 邵志刚, 李志海, 2014.印度板块与欧亚板块在兴都库什-帕米尔地区相互俯冲的动力作用分析.地球物理学报, 57(2):459-471. doi: 10.6038/cjg20140212 郑剑东, 1993.喀喇昆仑断层与塔什库尔干地震形变带.地震地质, 15(2):107-116, 195-196. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=dzdz199302001&dbname=CJFD&dbcode=CJFQ Blisniuk P. M., Strecker M. R., 1997. Quaternary oblique normal faulting in the Lake Karakul area, northern Pamir (Tajikistan): transfer of lateral escape along the Karakorum and Altyn Tagh faults? Geological Society of America, 29(6): 470. Tapponnier P., Mercier J. L., Armijo R., et al., 1981. Field evidence for active normal faulting in Tibet. Nature, 294(5840):410-414. doi: 10.1038/294410a0 Trifonov V. G., 1978. Late Quaternary tectonic movements of western and central Asia. Geological Society of America Bulletin, 89(7):1059-1072. doi: 10.1130/0016-7606(1978)89<1059:LQTMOW>2.0.CO;2 -
下载:
点击查看大图
计量
- 文章访问数: 96
- HTML全文浏览量: 49
- PDF下载量: 5
- 被引次数: 0
