| 黑龙江镜泊湖火山地区电性结构初步研究 |
| |
| 引用本文： | 朱仁学,付维洲,孟令顺,陈洪洲,赵谊.黑龙江镜泊湖火山地区电性结构初步研究[J].地震地质,2001,23(2):186-190. |
| |
| 作者姓名： | 朱仁学 付维洲 孟令顺 陈洪洲 赵谊 |
| |
| 作者单位： | 1. 吉林大学朝阳校区,
2. 黑龙江省地震局, |
| |
| 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 |
| 修稿时间： | 2001年2月1日 |
PRELIMINARY STUDY ON ELECTRIC STRUCTURE IN THE JINGBOHU VOLCANO AREA OF THE HEILONGJIANG PROVINCE |
| |
| Zhu Renxue,Fu Weizhou,Meng Lingshun.PRELIMINARY STUDY ON ELECTRIC STRUCTURE IN THE JINGBOHU VOLCANO AREA OF THE HEILONGJIANG PROVINCE[J].Seismology and Geology,2001,23(2):186-190. |
| |
| Authors: | Zhu Renxue Fu Weizhou Meng Lingshun |
| |
| 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 (relativ |
| |
| Keywords: | Jingbohu Volcano Magnetotelluric Resistivity Magma chamber |
| 本文献已被 CNKI 维普 万方数据 等数据库收录！ |
|
