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Abstract

It has been used resistivity geoelectric method with Wenner-Schlumberger configuration. The aim is to identify the distribution of iron ore located in the Ogowelevillage, Tolitoli regency. Research has been done using geoelectric method Wenner-Schlumberger configuration as well as data processing and data modeling using software EarthImager 2D in the 2D cross-sectional shape. Based on 2D modeling results resistivity value of the iron ore ranging from 55.8 to 156.2 Ωm. The existence of iron ore largelyspreadin South, West and East sites.

Keyword: geoelectric, resistivity, EarthImager 2D, iron ore

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How to Cite
Djuhaepa, A. P., Th. Musa, M. D., & sandra, sandra. (2015). Identification the distribution of iron ore used resistivity geoelectric method in the Ogowele Village, Tolitoli Regency. Gravitasi, 14(2). https://doi.org/10.22487/gravitasi.v14i2.5306

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