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地质力学学报:2007,13(1):78-85
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嘉峪关断裂晚第四纪新构造活动特征
(1.中国地质科学院地质力学研究所, 北京 100081;2.中国地震局兰州地震研究所, 甘肃, 兰州 730000)
LATE QUATERARY NEOTECTONIC MOVEMENT OF THE JIAYUGUAN FAULT
(1.Institute of Geomechanics, Chinese Academy of Geosciences, Beijing 100081;2.Lanzhou Institute of Seismology, China Seismological Bureau, Lanzhou 730000, Gansu)
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投稿时间:2007-02-05    
中文摘要: 嘉峪关活动断裂位于嘉峪关市,是与河西走廊中3个斜向隆起之一的嘉峪关-文殊山隆起密切相关的活动断裂,也是祁连山北缘-河西走廊活动断裂体系的组成部分。该断裂走向320°,呈线状延伸;断裂切错前白垩系、白垩系、新近系和上更新统;在剖面上断裂表现为南西盘上升、北东盘下降,平面上表现为明显的右行走滑运动。晚更新世晚期~全新世存在5期明显的新构造活动,分别发生于距今稍大于4.3ka、稍大于12.9ka、20.0~23.2ka、35.5~45ka和稍大于58.1ka。断裂粘滑活动为主,并具明显古地震特点。
Abstract:The Jiayuguan active fault is situated near Jiayuguan City.It is closely related to the Jiayuguan-Wenshushan uplift (which is one of the three uplifts in the Hexi Corridor:the JiayuguanWenshushan uplift in the western part of the Hexi Corridor, Yumushan uplift in the central part of the Hexi Corridor and Dahuangshan uplift in the eastern part of the Hexi Corridor)and is also a component part of the northern Qilian marginal-Hexi Corridor active fault system.The fault strikes N320°W and extends linearly for 20 km.It cuts the pre-Cretaceous, Cretaceous, Neogene and upper Pleistocene.In section, the southwestern block of the fault moves up, while the northeastern block moves down;in plan, it is marked by apparent right-lateral strike-slip motion.Five phases of neotectonic movement took place along the Jiayuguan fault during the latest Pleistocene to Holocene, i.e.at 4.3-4.5, 12.9-14.0, 20.0-23.2, 35.5-45 and 58.1 ka BP.The faulting was dominated by stick-slip movement and shows the distinctive characteristics of paleoearthquakes.
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基金项目:中国地质调查局地质调查项目(项目编号;水[2003]018-02)资助。
引用文本:
陈柏林,刘建生,张永双,等,2007.嘉峪关断裂晚第四纪新构造活动特征[J].地质力学学报,13(1):78-85.DOI:
CHEN Bai-lin,LIU Jian-sheng,ZHANG Yong-shuang,et al,2007.LATE QUATERARY NEOTECTONIC MOVEMENT OF THE JIAYUGUAN FAULT[J].Journal of Geomechanics,13(1):78-85.DOI:

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