地震地质 ›› 2018, Vol. 40 ›› Issue (5): 980-998.DOI: 10.3969/j.issn.0253-4967.2018.05.003
杨海波, 杨晓平, 黄雄南, 胡宗凯
收稿日期:
2017-11-05
修回日期:
2018-03-02
出版日期:
2018-10-20
发布日期:
2018-11-29
通讯作者:
杨晓平,研究员,E-mail:yangxiaoping-1@163.com
作者简介:
杨海波,男,1989年生,2016年于中国地震局地质研究所获构造地质学硕士学位,在读博士研究生,主要研究活动构造,E-mail:yanghaibo2015@gmail.com。
基金资助:
YANG Hai-bo, YANG Xiao-ping, HUANG Xiong-nan, HU Zong-kai
Received:
2017-11-05
Revised:
2018-03-02
Online:
2018-10-20
Published:
2018-11-29
摘要: 佛洞庙-红崖子断裂是祁连山北缘断裂带中构造活跃的断裂之一,断裂东段胡家台背斜区发育多种类型的构造,且部分断裂被证实在1609年M7 1/4红崖子地震中发生破裂,但复杂的地表破裂特征所反映的深部发震构造样式还不清楚。因此,文中选取了佛洞庙-红崖子断裂东段胡家台背斜区及附近多组活动构造为研究对象,利用差分GPS对变形的河流阶地、洪积扇等进行测量,并对背斜核部出露的地质剖面进行了实测,获得了不同类型构造的活动特征。结合已有穿过背斜的地震反射剖面,构建构造地貌与深部结构之间的对应关系,从而探讨地震的发震构造样式。研究表明,背斜区发育了胡家台背斜以及多条逆断裂或逆-走滑断裂,背斜为祁连山北麓逆断裂向N逆冲扩展形成,并伴随形成背斜东侧1条逆冲兼右旋走滑断裂和北侧另1条逆断裂,这些逆断裂或逆-走滑断裂为调节局部构造应变差异而产生。黄草坝探槽结果表明,1609年红崖子地震破裂了黄草坝T1阶地;再结合前人关于此次地震的野外考察和文献资料考证,认为1609年M7 1/4红崖子地震发生在祁连山山麓逆断裂上,地震至少破裂了NWW向山前F1、胡家台背斜东侧NNW向F2和EW向F3断裂,震源深度可能为8~22km。
中图分类号:
杨海波, 杨晓平, 黄雄南, 胡宗凯. 祁连山北缘佛洞庙-红崖子断裂胡家台背斜区构造变形——1609年M7 1/4红崖子地震构造样式[J]. 地震地质, 2018, 40(5): 980-998.
YANG Hai-bo, YANG Xiao-ping, HUANG Xiong-nan, HU Zong-kai. LATE QUATERNARY TECTONIC DEFORMATION AROUND THE HUJIATAI ANTICLINE ALONG THE EAST SEGMENT OF THE FODONGMIAO-HONGYAZI FAULT, NORTHERN QILIAN SHAN: AN INSIGHT ON THE SEISMOGENIC PATTERN OF 1609 HONGYAZI M7 1/4 EARTHQUAKE[J]. SEISMOLOGY AND GEOLOGY, 2018, 40(5): 980-998.
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