2017
DOI: 10.1071/eg15078
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Near-surface high resolution imaging of a metallogenic zone in the northern fringe of Dalma volcanics in eastern India using electrical resistivity tomography

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Cited by 8 publications
(4 citation statements)
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“…The three lithological units at depths ∼40, ∼25, and ∼15 m, respectively correspond to weathered intrusive/SGM, upper DVs and lower DVs and corroborate well with the major geological successions (table 1) obtained from drilling data at Parasi (22 • 57 N; 85 • 40 E) (figure 1) in the same geological domain as that of the study area; a proven gold prospective deposit (MECL 2010). The obtained results are in agreement with those of Adhikari et al (2016). They at a depth of ∼25 m obtained resistivity < 1 Ωm and attributed it to metallogeny coinciding to upper DVs.…”
Section: Resultssupporting
confidence: 91%
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“…The three lithological units at depths ∼40, ∼25, and ∼15 m, respectively correspond to weathered intrusive/SGM, upper DVs and lower DVs and corroborate well with the major geological successions (table 1) obtained from drilling data at Parasi (22 • 57 N; 85 • 40 E) (figure 1) in the same geological domain as that of the study area; a proven gold prospective deposit (MECL 2010). The obtained results are in agreement with those of Adhikari et al (2016). They at a depth of ∼25 m obtained resistivity < 1 Ωm and attributed it to metallogeny coinciding to upper DVs.…”
Section: Resultssupporting
confidence: 91%
“…Keating and Pinet (2011) have shown that, in general, the effect of bodies is less than the half of upward continuation height. ERT lines coincident with gravity and magnetic lines in the area show that the top of the ore body is ∼25 m and extends to a maximum depth of ∼50 m (Adhikari et al 2016). Following Keating and Pinet (2011) and keeping the ERT results in consideration, we have chosen the upward continuation at 150 m as regional anomaly both for gravity and magnetic studies.…”
Section: Data Acquisition and Processingmentioning
confidence: 99%
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