地震地质 ›› 2008, Vol. 30 ›› Issue (2): 454-463.DOI: CNKI:SUN:DZDZ.0.2008-02-011

• 研究论文 • 上一篇    下一篇

晚更新世以来黄土塬区临潼-长安断裂的活动性研究

李晓妮, 冯希杰, 戴王强, 师亚芹, 任隽, 李晋, 韩恒悦   

  1. 陕西省地震局|陕西省地震局 西安
  • 收稿日期:2008-06-20 出版日期:2008-06-20 发布日期:2008-06-20
  • 基金资助:

    国家发展和改革委员会发改投资“城市活断层试验探测”项目(20041138)资助

ACTIVITY OF THE LINTONG-CHANG AN FAULT IN LOESS TABLELANDS SINCE LATE PLEISTOCENE

  • Received:2008-06-20 Online:2008-06-20 Published:2008-06-20

摘要:

黄土塬区晚更新世风成黄土分布广、特征明显,与断裂关系直接。通过小鲍陂、桥沟、冢底村3个典型晚更新世断层剖面的仔细观察、测量和年代学工作,获得了白鹿塬、少陵塬、横岭塬3个黄土台塬上临潼-长安断裂晚更新世以来的活动性参数和区域地层的年代序列。研究结果表明,晚更新世以来临潼-长安断裂在白鹿塬段活动性最强,明显错断了黄土L1-2地层,而其两侧的少陵塬和横岭塬上,同时期断裂的活动性相对弱些。剖面中黄土L1-2及其以上地层被裂缝穿切的现象有可能说明,晚更新世中晚期以来临潼-长安断裂仍在活动,仅是强度有所减弱

关键词: 临潼-长安断裂, 黄土塬, 光释光测年, 晚更新世

Abstract:

The late Pleistocene aeolian loess distributes widely in the loess tableland area.It has obvious features and is directly related with faulting.By the observation,measurement and dating to three typical sections at Xiaobaopo,Qiaogou and Zhongdicun,this paper obtained the activity parameters of the Lintong-Chang an Fault since the late Pleistocene and the age stratigraphic sequence of the tablelands of Bailuyuan,Shaolingyuan and Henglingyuan.Research results show that the Bailuyuan tableland has experienced

Key words: Lintong-Chang an Fault, loess tableland, optical stimulated luminescence dating, late Pleistocene