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鲜水河断裂带全新世活动性研究进展综述

熊探宇 姚鑫 张永双

熊探宇, 姚鑫, 张永双, 2010. 鲜水河断裂带全新世活动性研究进展综述. 地质力学学报, 16 (2): 176-188.
引用本文: 熊探宇, 姚鑫, 张永双, 2010. 鲜水河断裂带全新世活动性研究进展综述. 地质力学学报, 16 (2): 176-188.
XIONG Tan-yu, YAO Xin, ZHANG Yong-shuang, 2010. A REVIEW ON STUDY OF ACTIVITY OF XIANSHUIHE FAULT ZONE SINCE THE HOLOCENE. Journal of Geomechanics, 16 (2): 176-188.
Citation: XIONG Tan-yu, YAO Xin, ZHANG Yong-shuang, 2010. A REVIEW ON STUDY OF ACTIVITY OF XIANSHUIHE FAULT ZONE SINCE THE HOLOCENE. Journal of Geomechanics, 16 (2): 176-188.

鲜水河断裂带全新世活动性研究进展综述

基金项目: 

中国地质调查局国土资源大调查项目 1212010914025

中国地质调查局国土资源大调查项目 1212011014035

详细信息
    作者简介:

    熊探宇(1985-), 男, 博士研究生, 地质工程专业。E-mail: xiongtanyu@126.com

  • 中图分类号: P642

A REVIEW ON STUDY OF ACTIVITY OF XIANSHUIHE FAULT ZONE SINCE THE HOLOCENE

  • 摘要: 鲜水河断裂带是中国西南山区一条现今活动强烈的大型地震断裂。本文在系统总结前人研究成果的基础上, 结合野外地质调查, 综述了鲜水河断裂带空间展布特征、活动性质及强度、历史地震地表破裂特征、地震危险性等方面的研究进展。前人研究结果表明, 鲜水河断裂带以惠远寺为界可分为两段, 进一步可细分为八段;断裂带全新世以来以左旋走滑为主, 兼具逆冲性质;整条断裂现今走滑活动速率约为10mm/a左右, 垂向变形在2mm/a以内;其中断裂带北西段活动速率为10~20mm/a, 南东段则小于10mm/a, 一般为5mm/a左右;断裂带地震活动频繁, 地震活动性北西段明显高于南东段, 强震迁移呈明显的跳跃式特征并具有原地复发性质;断裂带历史地震地表破裂特征与玉树地震所报道的地表破裂特征一致;断裂带地震危险性评价具很多不确定因素, 研究程度相对较低。

     

  • 图  1  广义的鲜水河断裂带空间展布图

    (据文献[14]修改)

    Figure  1.  A sketch map showing distribution of generalized Xianshuihe fault zone

    图  2  鲜水河断裂带空间展布特征

    (据文献[13])
    1.活动断裂; 2.前第四纪活动断裂; 3.第四纪盆地; 4.燕山晚期花岗岩; 5.澄江-晋宁期斜长花岗岩; 6.断裂编号: ①炉霍断裂; ②道孚断裂; ③乾宁断裂; ④雅拉河断裂; ⑤中谷断裂; ⑥色拉哈-康定断裂; ⑦折多塘断裂; ⑧磨西断裂; 7. 7.0级及以上地震震中和时间

    Figure  2.  A sketch map showing stretch of the Xianshuihe active fault zone

    图  3  鲜水河断裂带强震M-T图

    (据文献[35]修改)

    Figure  3.  A sketch map showing M-T of earthquakes(M≥5.0)in Xianshuihe active fault zone

    图  4  鲜水河断裂带M≥6地震时空关系图

    (据文献[26]修改)

    Figure  4.  A map showing the tempo-spatial relationship of earthquakes(M≥6.0)in Xianshuihe fault zone

    图  5  鲜水河断裂带地貌特征

    A-榆林乡南侧堰塞塘(NW); B-新榆林南侧石灰窑沟山脊左旋错动(NW); C–道孚南四十道班南东侧1981年道孚地震沟槽及鼓包地貌(SE); D-惠远寺北西侧沟槽地貌(SE); E-八美镇南侧构造石林地貌(E); F-松林口南东侧支沟左旋错动达290m(NE); G-道孚县恰叫村北1923年7.3级地震陡坎及鼓包(NW); H-折多山二台子道班南侧坡中槽地貌(SE)

    Figure  5.  A sketch map showing the geomorphology of Xianshuihe active fault zone

    图  6  甘孜-玉树断裂带玉树地震地表破裂特征

    (据文献[45])
    A-连续延伸的地震破裂(NW); B-右阶排列的地震地表破裂(NW); C-帐篷状构造(NW); D-地表破裂沿反向断坎发育(SE); E-禅古村逆冲走滑型断坎(SE); F-玉树县城区南部“X”型地裂缝(NE)

    Figure  6.  A sketch showing the surface rupture characteristics left in Yushu earthquake along Garzê-Yushu fault

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  • 收稿日期:  2010-05-17
  • 刊出日期:  2010-06-01

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