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首页> 外文期刊>International Journal of Geophysics >Integrating Apparent Conductance in Resistivity Sounding to Constrain 2D Gravity Modeling for Subsurface Structure Associated with Uranium Mineralization across South Purulia Shear Zone, West Bengal, India
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Integrating Apparent Conductance in Resistivity Sounding to Constrain 2D Gravity Modeling for Subsurface Structure Associated with Uranium Mineralization across South Purulia Shear Zone, West Bengal, India

机译:在印度西孟加拉邦南Purulia剪切带,将电阻率测深中的表观电导率整合到约束与铀矿化有关的地下结构的二维重力模型中

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摘要

South Purulia Shear Zone (SPSZ) is an important area for the prospect of uranium mineralization and no detailed geophysical investigations have been carried out in this region. To delineate the subsurface structure in the present area, vertical electrical soundings using Schlumberger array and gravity survey were carried out along a profile perpendicular to the SPSZ. Apparent conductance in the subsurface revealed a possible connection from SPSZ to Raghunathpur. The gravity model reveals the presence of a northerly dipping low density zone (most likely the shear zone) extending up to Raghunathpur under a thin cover of granitic schist of Chotanagpur Granite Gneissic Complex (CGGC). The gravity model also depicts the depth of the zone of density low within this shear zone at ~400m near Raghunathpur village and this zone truncates with a steep slope. Integration of resistivity and gravity study revealed two possible contact zones within this low density zone in the subsurface at depth of 40m and 200 m. Our study reveals a good correlation with previous studies in Raghunathpur area characterized by medium to high hydro-uranium anomaly.Thus the conducting zone coinciding with the low gravity anomaly is inferred to be a possible uraniummineralized zone.
机译:南普鲁里亚剪切带(SPSZ)是铀矿化前景的重要地区,该地区尚未进行详细的地球物理研究。为了描绘当前区域的地下结构,使用斯伦贝谢阵列进行垂直电测深,并沿垂直于SPSZ的剖面进行重力测量。地下的表观电导表明SPSZ与Raghunathpur之间可能存在联系。重力模型揭示了在Chotanagpur花岗岩片麻岩复合体(CGGC)的薄岩片岩薄覆盖下延伸到Raghunathpur的北倾低密度带(最可能是剪切带)的存在。重力模型还描绘了在拉古纳斯普尔村附近〜400m处该剪切带内低密度区域的深度,该区域以陡峭的斜面截断。电阻率和重力研究的综合表明,在40m和200m深度的地下低密度区内有两个可能的接触带。我们的研究表明,与拉古纳斯普尔地区以前的研究具有良好的相关性,其特征是中铀到高氢铀异常,因此推测与低重力异常相吻合的导电带可能是铀矿化带。

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