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崇礼—赤城含金剪切带具有独特的成矿地质演化历史。大约在印支—燕山期，水泉沟碱性杂岩体角闪二长岩及围岩发生了强烈的韧性剪切变形，并伴随复杂的面型→裂隙型碱→酸交代作用，演化出韧性剪切变形→变质（碱交代）岩石渐变过渡、逐步演化的角闪二长岩、二长岩、正长岩类岩石组合。而东坪、后沟、黄土梁、中山沟等石英脉—钾质蚀变岩型金矿，则是含金剪切带与碱性杂岩体复杂演化过程中逐步使金富集的最终（燕山期）产物。
Chongli - Akagi gold-bearing shear zone has a unique evolutionary history of metallogenic geology. During the Indosinian-Yanshanian period, strong ductile shear deformation occurred in the hornblende mafic rocks and the surrounding rocks of the Shuiquanigou alkaline complex, accompanied by complex facies → fissure type alkali → acid replacement, evolving toughness Shear deformation → metamorphic (alkali metamorphic) rock gradual transition, gradual evolution of hornblen amphibole, monzonite, monzonite, syenite rock group combination. However, the quartz vein-potash altered rock type gold deposits such as Dongping, Hougou, Loess Plateau, and Zhongshagou are the final phases of gold enrichment during the complicated evolution of gold-bearing shear zones and alkaline complexes Yanshan period) product.