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山阳-柞水矿集区是秦岭成矿带中主要矿集区之一,以出露大面积滨浅海相-三角洲相中-上泥盆统刘岭群为特征;区内除出露有大面积的晚三叠世的花岗质岩体,还发育晚侏罗世-早白垩世的小岩体/株/脉。空间上,山阳-柞水矿集区夹持于山阳-凤镇和商县-丹凤断裂之间,该盆地基底由北秦岭岛弧杂岩和山阳-凤镇构造混杂岩共同
The Shanyang-Zhashui ore district is one of the main ore-concentrating areas in the Qinling metallogenic belt. It is characterized by the appearance of large-area coastal shallow marine facies-delta facies-upper Devonian Liuling Group. In addition to the exposed large area Late Triassic granitic rock mass, and also the late Jurassic-Early Cretaceous small rock mass / plant / vein. Spatially, the Sanyang-Zhashui ore district is sandwiched between the Sanyang-Fengzhen and Shangxian-Danfeng faults, and the basement of this basin is jointly constructed by North Qinling Island arc complex and Sanyang-Fengzhen structural melange