摘要
位于太行山东麓邢邯地区的綦村铁矿，为一接触充填交代类型的磁铁矿床．实践证明，对本区构造特征与控矿构造规律的揭示与研究，是指导今后对该矿，区进行普查勘探和扩大远景的重要关键。为此。
The Ferrous mines in the Hanxing area in Hebei Province are magnetic deposits which are contact and replacement type. The main form of the structure in this mining area is folded structure developed in the Mid-Ordovician Series Majiagou stratum as the wall rock of diorite.The formation ways and expanding characteristics of the folded structure mentioned above are closely related to the strain field of regional structure and the activity of magmatic intrusion.The forms of ore body, Occurrenes, and enriched position of the mining area at Qi village are also controlled by folded structure, magma and moving direction of the ore current. Recogrizing and summing up these laws has great significance, for further searching for mineral resources.
