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Application of gravity imaging to geothermal exploration

机译:重力成像在地热勘探中的应用

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In the exploration of geothermal water in China,gravity method comes to be a major method because of its sensitivity to linear structure,especially to the fault,and the high efficiency to planimetric exploration.In order to improve the effect of gravity method exploration,imaging technology is often used for extracting the implicative information the survey data.Two successful case histories of applied gravity imaging technology to geothermal exploration are presented in this paper.Different kind of imaging technology,planar imaging and pseudo-depth imaging based on wavelet analysis,were used to respective case.In the case of planar imaging,the gravity anomaly was converted with a suited grid density to a value of the grayscale or brightness.Then we can display the gravity anomalies using the converted result.This kind of imaging technology was used to the first case history for mapping the fault and the boundary of the high-density rock.The pseudo-depth imaging was used to another case history for mapping the variation with its buried depth of a fault.1-d continuous wavelet analysis was used for generating the pseudo-depth value of the gravity profile.This is only an experiment although the result was concordant to which of the CSAMT in the same site.
机译:在我国的地热水勘探中,重力法由于对线性结构特别是断层敏感,对平面勘探具有很高的效率,因此成为主要方法。该技术常被用于提取勘测数据中的含意信息。本文介绍了将重力成像技术应用于地热勘探的两个成功案例。本文分别介绍了基于小波分析的平面成像和伪深度成像等不同的成像技术。在平面成像的情况下,将重力异常以合适的网格密度转换为灰度或亮度值,然后我们可以使用转换后的结果显示重力异常。使用了这种成像技术绘制出高密度岩石断层和边界的第一例历史记录断层隐伏深度变化的历史记录.1-d连续小波分析用于生成重力剖面的伪深度值。这只是一个实验,尽管结果与CSAMT中的哪个一致同一站点。

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