Multi-Elevations Upward Continuation Method to Depth Detection of the Main Crustal Layers in Western Desert of Iraq

Q3 Earth and Planetary Sciences Iraqi Geological Journal Pub Date : 2023-11-30 DOI:10.46717/igj.56.2e.20ms-2023-11-25
Ahmed Al-Banna, Hayder Majeed
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Abstract

The upward continuation technique was applied to the gravity and RTP magnetic data to obtain the residual anomalies maps in the western part of Iraq. Twelve upward elevation residual gravity maps and another twelve upward elevation residual RTP magnetic were determined using the same twelve upward continuation elevations. The applied upward elevations range from 1000 to 55000 m. The total range of the residual anomalies maps (Color Bar range) of gravity and RTP magnetic were plotted against the upward elevations. Five segments and four intersection points were obtained for the gravity and magnetic data. The trace of these intersection points on the upward elevation axis approximately indicate the following values 4.4-5, 12.8-13.5, 27-24, and 39-39.6 km. These values may indicate the depth of the following layer boundaries, the Burj Formation ( Mid-Cambrian), basement, mid layer in the basement rocks, and the Moho depth. The authors believe it is possible to apply the upward continuation to find the main layers which show abrupt change in the physical properties
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伊拉克西部沙漠主要地壳层深度探测的多高程向上延续方法
对重力和 RTP 磁数据采用了向上延续技术,以获得伊拉克西部的残余异常图。利用同样的 12 个向上延续高程,绘制了 12 幅向上高程残余重力图和另外 12 幅向上高程残余 RTP 磁图。重力和 RTP 磁性残余异常图的总范围(彩条范围)与上升标高相对应。得出了重力和磁力数据的五个区段和四个交点。这些交点在上升标高轴上的轨迹大致显示了以下数值:4.4-5、12.8-13.5、27-24 和 39-39.6 千米。这些值可能表示以下地层边界的深度:Burj Formation(中寒武纪)、基底、基底岩石中层以及莫霍深度。作者认为,可以应用向上延续的方法来寻找物理性质发生突变的主要地层
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来源期刊
Iraqi Geological Journal
Iraqi Geological Journal Earth and Planetary Sciences-Geology
CiteScore
1.80
自引率
0.00%
发文量
152
审稿时长
7 weeks
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