摘要
The Gaocaiban copper-polymetallic deposit in Datian county was discovered in the three early Triassic Wenbinshan formation and was obviously controlled by NE faulted structures in the east wing of Kunshan syncline.14 copper polymetallic ores have been discovered.The ore body is complex morphology,exists in veins overall and local in lenticular.The deposit belong to the hydrothermal filling and metasomatic vein deposit with dip angle and continuous mineralization.The elements of Shisunqi Cu-Pb-Zn-Mo integrated soil anomaly have a better telescoping in the south deposit.The anomaly is high in concentrations,is countinuous in distribution,is large in size and the contraction center of the anomalies is obvious.In conclusion,there are good ore-forming geological conditions in the area,so there will still be the lare-scale hidden copper polymetallic deposit to be found in the soil anomaly area of the west wing and South-East of east wing of Kunshan Syncline.