Application of the CSAMT Method for Exploring Deep Coal Mines in Fujian Province, Southeastern China

Abstract

Coal reserve volume in Fujian Province, China, ranks third among the nine provinces in southern China. Over the past decades, most coal mines in uncovered and semi-covered coal strata have been explored and developed. Present exploration mainly focuses on deep coal strata, which are generally covered by older strata and volcanic strata. Because of the terrain and deep targets, seismic prospecting is difficult. The major coal-containing strata that can be excavated in Fujian are within the Tungtzeyan Formation of the Lower Permian Series. The thickness of this formation is greater than [Formula: see text]. The CSAMT (controlled source audio frequency magnetotelluric) method isused to delineate four deep coal strata units. The aim of this prospecting is to delineate the upper and lower boundaries of the stratum containing the coal units. The prospecting target depth is approximately [Formula: see text], which required a frequency range between [Formula: see text] and [Formula: see text] to provide sufficient data coverage. The distance from the transmitter to the survey line was [Formula: see text], with a transmitting current of [Formula: see text] and voltage of [Formula: see text]. The time synchronization between the transmitter and receiver was controlled by a global positioning system. Major static problems were encountered during the CSAMT survey. Both terrain and static corrections were applied during data processing, which smoothed the inverted results for better interpretation. Comparison of the CSAMT interpreted results with available engineering geology information shows a clear difference in electrical properties between coal stratum, upper old stratum, red-beds and volcanic strata. The CSAMT method is useful in identifying the coal strata under these geological conditions.