Soil Geochemical Anomaly Characteristics in the East Area of Dasaituo and Its Exploration Effect

详细信息   
摘要

The east area of Dasaituo in Inner Mongolia is located in east section of Xilinhaote-Dongwuqi polymetallic mineralization zone with favorable ore-forming condition but less surface outcrop and largely overlaid by Quaternary system causing difficulty in ore prospecting. Soil geochemical exploration has outlined three S-N striking anomaly zones lying from west to east, based on element combination characteristics and zoning theory, signaling that east side of No and anomaly zone is in front halo of the orebody, with anomaly zone occurring in middle front of the orebody and west side of anomaly zone occurring in the end halo of orebody, forming clear horizontal zoning of the anomaly, and presuming a variation trend of ore erosion from shallow to deep.

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