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太和铁矿是攀西四大钒钛磁铁矿典型矿床之一。多层钒钛磁铁矿体在华力西期太和层状基性超基性岩体中上部呈层状、似层状产出平行产出,根据赋矿岩性和矿石特征,可分为3个矿带9个矿组。岩矿体走向北东倾向南西,控制长2600 m、最大斜深1940m,矿体(层)累计厚194.09～557.03m。走向上由东到西矿体累计厚度逐降低,倾向上,由浅到深矿层逐步归并复合,形成厚度大,矿层结构简单的工业矿体。整装勘查在矿区深部新增资源量:铁矿石98680万吨、TiO29539万吨、V2O5228万吨。预测深部钒钛磁铁矿资源潜力巨大。
Taihe iron ore is Panxi four vanadium titanium magnetite one of the typical deposits. The multi-layered vanadium-titanium magnetite ore bodies are stratified in the upper part of the Taihe-stratiform overlying basic ultramafic rocks in the Haryclical period, and the stratiform output is parallel to each other. According to the ore-bearing lithology and ore characteristics, the multi-layered vanadium- 3 mine with 9 mines. The ore body moves towards the north-easterly direction to the southwest with a control length of 2,600 m and a maximum depth of 1940 m. The ore body (layer) accumulates in thickness from 194.09 to 557.03 m. From the east to the west, the cumulative thickness of the ore body decreases gradually. According to the tendency, the ore body gradually merges from the shallow to the deep ore and forms a complex ore body with large thickness and simple orebody structure. The survey of new assets in the mining area to add new resources: 986.8 million tons of iron ore, TiO2, TiO2, TiO2, TiO2 Predict the deep potential of vanadium-titanium magnetite resources.