求翻译成英文,在线等激发极化法,简称激电法,是以地下岩、矿石在人工电场作用下发生的物理和电化学效应（激发极化效应）差异为基础的一种电法勘探方法.其可以分为时间域激电法和频率

求翻译成英文,在线等激发极化法,简称激电法,是以地下岩、矿石在人工电场作用下发生的物理和电化学效应（激发极化效应）差异为基础的一种电法勘探方法.其可以分为时间域激电法和频率
求翻译成英文,在线等
激发极化法,简称激电法,是以地下岩、矿石在人工电场作用下发生的物理和电化学效应（激发极化效应）差异为基础的一种电法勘探方法.其可以分为时间域激电法和频率域激电法.在19世纪人们已经发现岩石具有激发极化效应,但直到20世纪40年代才将它应用到物探中来.到20世纪60年代以后,激发极化法成为寻找各种金属矿床的主要物探方法,并取得了显著的效果.目前激发极化法已经广泛应用于国民生产中的各个方面.中间梯度装置和偶极装置是激电法最常用的两种装置,并且各自有其优点和缺点.本文在阐述激发极化法的研究历史、发展情况及应用现状基础上,结合已有的测区地质概况资料及其地理物理特征,重点对所研究金属矿区激电勘探资料解释,对结果进行合理的推断.工作方式采用激电中梯装置和偶极装置,对所采集数据进行处理成图,分析激电异常,进行综合解释.

求翻译成英文,在线等激发极化法,简称激电法,是以地下岩、矿石在人工电场作用下发生的物理和电化学效应（激发极化效应）差异为基础的一种电法勘探方法.其可以分为时间域激电法和频率
Induced polarization method, referred to as IP, is the underground rock, ore occurs in the artificial electric field and the physical and electrochemical effects (IP) a kind of electrical prospecting method based on differences. It can be divided into time domain induced polarization method and the frequency domain IP method. In nineteenth Century, it has been found that rock has the effect of induced polarization, but until twentieth Century 40 years before it is applied to the geophysical prospecting in. In twentieth Century 60 years later, induced polarization method has become the main geophysical methods for all kinds of metal deposits, and has achieved significant results. All aspects of the current induced polarization method has been widely used in the production of. Intermediate gradient device and dipole device is IP two device most in use, and each has its advantages and disadvantages. In this paper, the induced polarization method research history, development and the application present situation foundation, combined with geological data and geophysical characteristics of existing, focus on the explanation of the metal mine IP prospecting data research, carries on the reasonable extrapolation of results. Work with IP intermediate gradient device and dipole device, the acquired data mapping, analysis of IP anomaly, comprehensive interpretation