高密度电阻率法在雄安新区浅表古河道精细化探测中的应用研究

doi:10.11720/wtyht.2023.1245

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Abstract

To explore in detail superficial paleochannels in Xiong'an New Area,this study investigated two profiles in the study area using the high-density resistivity method based on previous remote sensing.The interpretation results were verified through drilling.The distribution range of the paleochannels that was delineated using the high-density resistivity method was more accurate than that obtained from remote sensing.This study determined that the superficial paleochannels in the study area exhibit curved,tortuous,and braided planar distribution,achieving excellent application performance in the detailed exploration of superficial paleochannels.This study provided a new idea for future exploration and study of superficial paleochannels and can be used as a reference for the selection of methods used to investigate paleochannels in similar geological conditions.

Key words： high-density resistivity method shallow paleochannel detailed detection borehole Xiong’an new area

Received: 01 June 2022 Published: 24 February 2023

ZTFLH:

P631.4

Corresponding Authors: CAO Zhan-Ning E-mail: syj95123@163.com;guffawn@foxmail.com

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	Articles by authors
	Yong-Jun SU
	Zhan-Ning CAO
	Geng-Xin ZHAO
	Xiang-Yun HU
	Jian FAN
	Jing ZHANG
	Cui-Song FAN
	Zhong-Feng HUANG

Cite this article:

Yong-Jun SU,Zhan-Ning CAO,Geng-Xin ZHAO, et al. Application of the high-density resistivity method in detailed exploration of superficial paleochannels in Xiong'an New Area[J]. Geophysical and Geochemical Exploration, 2023, 47(1): 272-278.

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https://www.wutanyuhuatan.com/EN/10.11720/wtyht.2023.1245 OR https://www.wutanyuhuatan.com/EN/Y2023/V47/I1/272

Statistics of physical parameters of rock(soil)layer in the study area

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The survey line map of the study area(revised from reference[9])

Comparison of test inversion results of high-density resistivity method with different point spacings of L0 line

Statistics of sand thickness of paleochannels,upper roof and lower floor by inversion interpretation of high-density resistivity method with different point spacings

The geological column of boreholes

Inversion result and interpretation of L1 high density resistivity method

Inversion result and interpretation of L2 high density resistivity method

Distribution range of shallow paleochannels by remote sensing interpretation and the high density resistivity method interpretation
a—distribution range of paleochannels by remote sensing interpretation;b—distribution range of shallow paleochannels by geophysical interpretation

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