依兰—伊通断裂新构造活动规律分析

翟明见, 朱光, 刘备, 顾承串, 张帅, 林少泽, 宋利宏. 依兰—伊通断裂新构造活动规律分析[J]. 地质科学, 2016, 51(2): 594-618. doi: 10.12017/dzkx.2016.019
引用本文: 翟明见, 朱光, 刘备, 顾承串, 张帅, 林少泽, 宋利宏. 依兰—伊通断裂新构造活动规律分析[J]. 地质科学, 2016, 51(2): 594-618. doi: 10.12017/dzkx.2016.019
Zhai Mingjian, Zhu Guang, Liu Bei, Gu Chengchuan, Zhang Shuai, Lin Shaoze, Song Lihong. Analysis on neotectonic activity of the Yilan-Yitong fault[J]. Chinese Journal of Geology, 2016, 51(2): 594-618. doi: 10.12017/dzkx.2016.019
Citation: Zhai Mingjian, Zhu Guang, Liu Bei, Gu Chengchuan, Zhang Shuai, Lin Shaoze, Song Lihong. Analysis on neotectonic activity of the Yilan-Yitong fault[J]. Chinese Journal of Geology, 2016, 51(2): 594-618. doi: 10.12017/dzkx.2016.019

依兰—伊通断裂新构造活动规律分析

详细信息
    作者简介:

    翟明见,男,1990年10月生,硕士研究生,构造地质学专业.E-mail:zmjqyfw@163.com

    通讯作者: 朱光,男,1959年3月生,博士,教授,构造地质学专业.E-mail:zhuguang59@hotmail.com
  • 中图分类号: P542

Analysis on neotectonic activity of the Yilan-Yitong fault

More Information
    Corresponding author: Zhu Guang
  • 作为郯庐断裂带北段主干的依兰—伊通断裂, 其新构造活动性与活动规律仍然存在不同的认识.本次工作通过详细的野外调查, 发现该断裂内活断层广泛存在, 由东、西两支北东走向的主干活断层构成, 沿着古近纪地堑边界断层发育.这些活断层主要呈破碎型结构, 多为逆右行平移活动.通过对这些活断层一系列实测擦痕反演应力场, 显示它们多是在东西向挤压中活动的, 而现今应力场转变为北东东—南西西向区域性挤压.依据本次野外观察与14 C定年, 并结合前人定年结果与近代地震分布, 表明依兰—伊通西支活断层的最新活动时代为全新世与晚更新世相间, 而东支活断层的最新活动时代主要为早-中更新世.依兰—伊通断裂内活断层显示了明显的差异性活动, 表现为西支的活动强度明显大于东支, 西支的最新活动时代皆晚于东支, 沿走向上活动性强、弱相间与最新活动时代不断变化, 以及近代地震活动不均一分布.它们沿走向上的分段性、差异性活动主要是因为被一系列北西向断层切断所致.
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出版历程
收稿日期:  2015-07-11
修回日期:  2015-11-25
刊出日期:  2016-04-25

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