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Mineral Potential of the Dhanjori Metavolcanics, East Singhbhum, Jharkhand

机译:贾坎德邦东辛格布姆Dhanjori Metvolonics的矿物潜力

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Deep Electrical Profiling (DEP) has proved to be very useful in identifying buried conductive anomalies in Dhanjori basin. 2-D modeling of such anomalies indicated a near vertical conductive body (80 ohm m) within the metabasics of Dhanjoris. A deep stratigraphic cum structural borehole drilled vertically upto a depth of 768 m over this anomaly zone revealed flat lying metavolconic assemblages grading from acidic to ultra basic in composition with interlayering of tuff and sediments. At least four different flows have been identified following the classical top and bottom criteria followed in stratigraphy. The bore hole lithology is in itself a revealation as it is different from the expected lithostratigraphy of Dhanjori basin. The metabasics are highly sheared and striated and the propensity of shearing increases with depth. Deep Electrical Sounding (DES) has been successful in estimating the thickness of the lithopackage which is within 1 km. SP, resistance, natural gamma ray logs run up to 750 m deptindicate 37 distinct conductive zones, varying from a fraction of a meter to several meters. Some of these are sulphides with pyrite, chalcopyrite, covellite and arsenopyrite assemblages. Density and chargeability values measured in the laboratory on selected core samples corroborate the above findings.
机译:事实证明,深电剖析(DEP)对于识别Dhanjori盆地的地下导电异常非常有用。此类异常的二维建模表明,在Dhanjoris的次生地层内接近垂直的导电体(80 ohm m)。在该异常区域上垂直钻探深达768 m的深层地层兼结构性钻孔,发现平躺的准火山岩组合物从酸性逐渐过渡到超碱性,凝灰岩和沉积物夹层。遵循地层学中的经典顶部和底部标准,至少确定了四种不同的流动。钻孔岩性本身就是一个发现,因为它与Dhanjori盆地预期的岩石地层学有所不同。亚基被高度剪切和横纹,剪切的倾向随深度增加。深度电测深(DES)已成功地估计了1公里以内的岩石包装的厚度。 SP,电阻,天然伽马射线测井记录长达750 m,确定了37个不同的导电区域,范围从一米到几米不等。其中一些是硫化物,包括黄铁矿,黄铜矿,陨石和毒砂组成。在实验室中对选定的核心样品测得的密度和荷电率值证实了上述发现。

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