江英豪, 王成虎, 刘卓岩, 张杰. 2016: 五大连池火山区域古应力场的初步研究基于火山口模式反演. 工程地质学报, 24(s1): 160-166. DOI: 10.13544/j.cnki.jeg.2016.s1.024
    引用本文: 江英豪, 王成虎, 刘卓岩, 张杰. 2016: 五大连池火山区域古应力场的初步研究基于火山口模式反演. 工程地质学报, 24(s1): 160-166. DOI: 10.13544/j.cnki.jeg.2016.s1.024
    JIANG Yinghao, WANG Chenghu, LIU Zhuoyan, ZHANG Jie. 2016: PRELIMINARY STUDY OF ANCIENT STRESS FIELD IN WUDALIANCHI VOLCANIC REGION-BASED ON INVERSION OF CRATER MODEL. JOURNAL OF ENGINEERING GEOLOGY, 24(s1): 160-166. DOI: 10.13544/j.cnki.jeg.2016.s1.024
    Citation: JIANG Yinghao, WANG Chenghu, LIU Zhuoyan, ZHANG Jie. 2016: PRELIMINARY STUDY OF ANCIENT STRESS FIELD IN WUDALIANCHI VOLCANIC REGION-BASED ON INVERSION OF CRATER MODEL. JOURNAL OF ENGINEERING GEOLOGY, 24(s1): 160-166. DOI: 10.13544/j.cnki.jeg.2016.s1.024

    五大连池火山区域古应力场的初步研究基于火山口模式反演

    PRELIMINARY STUDY OF ANCIENT STRESS FIELD IN WUDALIANCHI VOLCANIC REGION-BASED ON INVERSION OF CRATER MODEL

    • 摘要: 研究表明区域地应力场会影响火山岩脉群分布及火山口排列。通常情况下火山口排列与喷发时区域最大水平主应力方向平行,与最小水平主应力垂直。本文结合国外较成熟的火山口排列调查法,以我国黑龙江省的五大连池为研究对象。在遥感图像和火山口年代数据的基础上,经过图像处理,火山群构造图分析及火山群线性模式处理后反演出五大连池的区域地应力场。结果表明:此方法反演出的五大连池最大水平主应力方向是北东向,与震源机制解的应力方向信息相符。国外已对该方法开展了较全面的研究,然而国内这方面几乎没人研究。反演结果论证了方法的实用性,可以将方法应用在国内典型火山群区域,补充区域的应力方向信息。

       

      Abstract: Research shows that regional stress field affects the distribution of volcanic dikes and craters. Normally, the arrangement of craters parallels to the direction of maximum horizontal principal stress and verticals to the minimum horizontal principal stress. Combining the foreign method of crater survey, this paper studys wudalianchi in heilongjiang province. In the basis of remote sensing images and volcanic data, this paper processes images, analyses volcanic structure diagram and processes linear mode of volcanic craters to inverse wudalianchi regional stress field. Result shows that wudalianchi maximum horizontal principal stress direction is NE.this result coincides with the stress direction information of focal mechanism solution. Abroad has conducted a comprehensive study of the method, however the few domestic research. Inversion result demonstrates that the method is practical, so we can apply this method in the region of the domestic typical volcanoes to compensate regional stress direction information

       

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