首页> 外文期刊>Journal of geophysics >Identification of Subsurface Structures and their Inferences from Regional Magnetic (Total Field) Survey for loci of Kimberlite Pipe Rocks in the Western part of Anantapur and Adjoining Areas, Andhra Pradesh.
【24h】

Identification of Subsurface Structures and their Inferences from Regional Magnetic (Total Field) Survey for loci of Kimberlite Pipe Rocks in the Western part of Anantapur and Adjoining Areas, Andhra Pradesh.

机译:Andapur和毗邻地区西部磁性管道岩石岩体区域磁性(总场)调查识别及其推论及其邻近地区。

获取原文
获取原文并翻译 | 示例
       

摘要

The Magnetic (Total Field) survey has recorded characteristic magnetic responses over different litho units with significant contour pattern trending in NW-SE, NE-SW, N-S and E-W directions in the form of magnetic linears, breaks, gradients and circular and bipolar anomalies, indicating fault/contact in between the formations which are responsible for the formation of cross structural trends. The magnetic map has shown a variation of 930 nT ranging from -561 nT to +369 nT in the area. The magnetic map has clearly traced the Ramagiri- Pēnakacherla schist belt from Kuderu to Ramagiri in the form of linear feature aligned in N-S direction with moderate variation of -50nT to 100nT and sparse contour pattern. The rocks exposed in the area are of PGC, Dharwar, schist belt, mafic gabbro/dolerite dykes and small plutons of pink/grey hornblende biotite granite. The general trend of formations is in NNW-SSE to N-S direction with moderate to steep dips. The magnetic map has delineated a few inferred structural features. The intersection of NW-SE, NE-SW and E-W magnetic linears observed around Alamuru, Raptadu, Kuderu, Atmakuru, Ramasagaram, Golla, west of Sirpi and near Maddelacheruvu, Known as "Joints" needs further detailed study from the point of mineral exploration as most of the kimberlite bodies are identified near these intersections. Three test pits were opened over the anomaly zones and the analysis of the rock/soil samples were quite encouraging for the path finder elements of Kimberlite clan of rocks. A few blocks were recommended for further detailed geophysical surveys.
机译:磁性(总场)测量在不同的Litho单元上记录了具有磁性线性,断裂,梯度和圆形和双极异常形式的NW-SE,NE-SW,NS和EW方向的显着轮廓图案的特征磁响应。指示在形成交叉结构趋势的形成的地层之间的故障/接触。磁性图已经示出了该地区的930nt至-561nt至+369 nt的变化。磁性图已清楚地将ramagiri-pēnakacherlaschist皮带从Kuderu以N-S方向对准的线性特征的形式跟踪,以适度的-50nt至100nt和稀疏轮廓图案。该地区暴露的岩石是PGC,Dharwar,Schist皮带,MAFIC Gabbro / Dolerite Dykes和粉红色/灰色Hornblende Biotite花岗岩的小型砖。地层的一般趋势是NNW-SSE到N-S方向,中度浸入陡坡。磁性图已经描绘了几种推断的结构特征。在Alamuru,Raptadu,Kuderu,Atmakuru,Ramasagaram,Golla,Siridi西部和Maddelacheruvu西部观察到的NW-SE,Ne-SW和EW磁性线性的交点,称为“关节”,从矿物勘探中进一步详细研究由于大多数金伯拉特身体被识别在这些交叉口附近。在异常区域上打开三个测试坑,对岩石氏菌族氏族的路径探测器元素相当令人鼓舞。建议几个块用于进一步详细的地球物理调查。

著录项

相似文献

  • 外文文献
  • 中文文献
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号