SEISMOLOGY AND GEOLOGY ›› 2001, Vol. 23 ›› Issue (2): 186-190.

• Brief Report • Previous Articles     Next Articles

PRELIMINARY STUDY ON ELECTRIC STRUCTURE IN THE JINGBOHU VOLCANO AREA OF THE HEILONGJIANG PROVINCE

Zhu Renxue1, Fu Weizhou1, Meng Lingshun1, Chen Honzhou2, Zhao Yi2   

  1. 1. Jilin University, Chaoyang School-Section, Changchun 130026;
    2. Seismology Bureau of Heilongjiang, Harbin 150090
  • Received:2001-01-31 Revised:2001-02-28 Online:2001-06-05 Published:2009-10-26

黑龙江镜泊湖火山地区电性结构初步研究

朱仁学1, 付维洲1, 孟令顺1, 陈洪洲2, 赵谊2   

  1. 1. 吉林大学朝阳校区, 长春130026;
    2. 黑龙江省地震局, 哈尔滨150090

Abstract: In the Jingbohu volcano area of Heilongjiang province, MT measurement of 30 sites has been done. The results are as follows. The explored zone is non 1D structure. The central part is 2D structure. Its strike direction is north-east. In the vertical orientation there are three resistivity layers. Upside resistivity is middling value. Middle is high value. Bottom is low value. The surrounding resistivity of the explored area is larger. In the middle part of the explored area there is low resistivity (relative to periphery) vertical columniation of which the section is not regular, and its strike direction is north-east, and its resistivity has a “middle-high-low” style from the top to the bottom.

Key words: Jingbohu, Volcano, Magnetotelluric, Resistivity, Magma chamber

摘要: 在黑龙江镜泊湖火山地区做了30个点的大地电磁测深工作。结果表明:测区为非一维结构,中部为二维结构,走向为北东向。上下大致可分为3个电性层,电阻率上部为中阻,中部为高阻,下部为低阻。测区四周电阻率高,中部有一个截面不规则的北东向拉长的低阻立式柱状体,该柱体的电阻率从上到下也呈“中-高-低”形式。

关键词: 镜泊湖, 火山, 大地电磁测深, 电阻率, 岩浆囊