重力法在探测基岩埋深中的应用

Application of Gravity Method to the Detection of Depth of Bedrock

本文介绍了如何用重力法探测被第四系和第三系松散层覆盖下的基岩埋深。在克服不利的地电条件和节省时间与费用方面重力法比电法更优越一些。

Two practical cases of detecting depth of bedrock covered by Quaternary and Neocene by using gravity method are presented in this article. In the respect of overcoming disadvantageous condition of earth current and saving of time and costs, gravity method is better than resistivity method.