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赛什塘铜矿床系1955年由群众报矿发现。随即进行了地质调查、地面磁测以及少量的槽、坑探工作。因地表品位低、厚度小,未作深部了解。 1967年,我队对该点进一步进行地质物探检查工作,发现地质表矿化虽不好,但地磁异常长达三千五百米,宽几百米,并处于有利的地质构造部位。1969年经深部验证,见到了较好的工业矿体,现已探明为一中等规模的铜矿床。
Saishitang copper deposit was discovered by the masses in 1955. A geological survey, ground magnetometry and a few troughs and pit inspections were carried out. Due to the surface grade is low, the thickness is small, did not make a deep understanding. In 1967, our team conducted further geophysical and geochemical survey at this site and found that although the mineralization of the geological table is not good, the geomagnetic anomaly is as high as 3,500 meters and a few hundred meters wide and is in a favorable geological structure. After deep verification in 1969, the better industrial ore body was seen and it has been proved to be a medium-sized copper deposit.