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引用本文:张晓亮,张磊,王志辉,白凌燕,蔡向民,张敬江,刘振华,张悦泽,倪敬波. 基于磁性地层和沉积地层特征对北京市南口—孙河断裂活动性评估[J]. 中国地质, 2020, 47(3): 868-878.
ZHANG Xiaoliang,ZHANG Lei,WANG Zhihui,BAI Lingyan,CAI Xiangmin,ZHANG Jingjiang,LIU Zhenhua,ZHANG Yueze,NI Jingbo. Evaluation of the Nankou-Sunhe fault activity in Beijing based on the characteristics of magnetic strata and sedimentary strata[J]. Geology in China, 2020, 47(3): 868-878(in Chinese with English abstract).
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基于磁性地层和沉积地层特征对北京市南口—孙河断裂活动性评估
张晓亮1,2, 张磊1, 王志辉3, 白凌燕1, 蔡向民1, 张敬江2, 刘振华1, 张悦泽1, 倪敬波1
1.北京市地质调查研究院, 北京 100195;2.北京大学地球与空间科学学院, 北京 100871;3.中国地质科学院, 北京 100037
摘要:
南口—孙河断裂是北京平原区一条重要的活动断裂,也是渤海—张家口断裂带的组成部分。本文通过开展钻探和样品测试(古地磁和14C测年)分析工作,利用沉积相分析和磁性地层学技术方法建立钻孔沉积地层的磁极性年代序列,并对南口—孙河断裂北段进行第四纪以来活动性进行分析和研究。结果表明:南口—孙河断裂北段第四纪以来的活动性变化特征表现为早更新世早期(2.58~0.99 Ma)活动性由强转弱,在早更新世末期(0.99~0.78 Ma)再次转强;中更新世(0.78~0.126 Ma)活动性转弱;晚更新世至全新世(0.126 Ma至今)活动性再次加强。这一规律与北京西山隆升基本特征吻合,活动性总体表现“强-弱-加强”的特点。
关键词:  南口—孙河断裂  磁性地层  沉积相  活动速率  沉积速率  地质调查工程  北京
DOI:10.12029/gc20200322
分类号:P546;P542.3
基金项目:中国地质调查局项目(DD20179611,12120113012000)资助。
Evaluation of the Nankou-Sunhe fault activity in Beijing based on the characteristics of magnetic strata and sedimentary strata
ZHANG Xiaoliang1,2, ZHANG Lei1, WANG Zhihui3, BAI Lingyan1, CAI Xiangmin1, ZHANG Jingjiang2, LIU Zhenhua1, ZHANG Yueze1, NI Jingbo1
1.Beijing Institute of Geological Survey, Beijing 100195, China;2.School of Earth and Space Sciences, Peking University, Beijing, 100871, China;3.Chinese Academy of Geological Sciences, Beijing 100037, China
Abstract:
Nankou-Sunhe fault is one of most importance active faults in Beijing plain and one part of Bohai Bay-Zhangjiakou fault belts. This paper builds magnetic polarity chronology of borehole sedimentary strata based on magnetic stratigraphy and sedimentology with drilling and paleomagnetism and 14C samples testing, analyses and discusses the active features of NankouSunhe fault in the north segment since Quaternary period. The research indicates that:the fault activity changed from high to low intensity in the early stage of early Pleistocene(2.58-0.99 Ma)and turned into high intensity in the late stage of early Pleistocene (0.99-0.78 Ma), from strong to low intensity again in the Middle Pleistocene (0.78-0.126Ma), and then from low to high again intensity (0.126 Ma-present). This active feature is consistent with west mountain of Beijing uplift which shows the characteristics of high-low-high intensity.
Key words:  Nankou-Sunhe fault  magnetic stratigraphy  sedimentary facies  activity rate  deposition rate  geological survey engineering  Beijing