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本文想就太行山东麓矽卡岩型铁矿的成矿地质特征提出一些看法和意见。区域地层、构造及火成岩活动本区位于山西台背斜与河淮台向斜的过渡地带,具有地台边缘构造的特征。区域内除前震旦纪古老变质岩系之外,以古生代沉积岩层为主,局部有三迭纪地层产出。在低洼地带,第三纪砾石层及第四纪黄土分布甚广。
This article would like to put forward some opinions and opinions on the mineralization geological characteristics of the skarn type iron ore in the east foot of the Taihang Mountains. Stratigraphy, tectonics and igneous activity The area is located in the transitional zone between the anticline and the Huanghuai syncline in Shanxi Province, and is characterized by the marginal structure of the platform. In addition to the former Pre-Sinian metamorphic rocks in the region, the Paleozoic sedimentary rock-based, locally Triassic strata output. In low-lying areas, Tertiary gravel and Quaternary loess are widely distributed.