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Geophysical Studies for Configuring the Bedrock Profile along Jhiri Dam Alignment, Par-Tapi-Narmada Link Project, Nasik District, Maharashtra

机译:沿jhiri坝对齐配置基岩轮廓的地球物理学研究,帕拉·纳马达联赛项目,纳西克区,马哈拉施特拉

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摘要

The paper presents the results of geophysical surveys conducted along the Jhiri dam alignment in district Nasik, Maharashtra at the request of the Par-Tapi-Narmada Link Project of National Water Development Agency (NWDA). National Water Development Agency (NWDA) is the first Water Resources Management Scheme involving interbasin transfer of Par, Nar, Tan, Ambika, Khapri and Purna rivers through Tapi (Ukai reservoir) and Narmada (Sardar Sarovar reservoir) to Kutch region in the state of Gujarat. Under this programme, geophysical surveys employing seismic, electrical resistivity and magnetic techniques were conducted for the delineation of bedrock configuration and the geological structural features, if any, present in the vicinity of the dam alignment. The Jhiri dam site is located across river Par near village Jhiri which is situated about 3 km west of village Jhiri in Nasik district. The depth to the bedrock at dam site varies between 2.9 m and 20 m showing P-wave velocity ranging between 5000 to 5100 m/s.
机译:该论文介绍了马哈拉施特地区纳西克区纳西克区吉尔里坝对齐的地球物理调查的结果,应当要求国家水开发机构(NWDA)的Par-Tapi-Narmada Link项目。国家水开发机构(NWDA)是涉及通过Tapi(Ukai Chockoir)和NARMADA(Sardar Sarovar Chockoir)到kuch地区的Tapi(Ukai水库)和Purna Rivers interbasin转让的水资源管理计划。古吉拉特邦。在该程序下,进行采用地震,电阻率和磁技术的地球物理调查,用于描绘坝体对准附近的基岩配置和地质结构特征,如果有的话。 Jhiri Dam Site位于江边河附近的河流局,距离纳西克区贾吉岛以西约3公里处。坝址的基岩的深度在2.9米和20米之间变化,显示P波速度范围为5000至5100 m / s。

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