摘要
金青顶矿床地处牟（平）—乳（山）金成矿带内，将军石—曲河庄断裂为区内一级控矿构造，其成生经历了多期次的构造演化，由于构造—成矿期次的不同，产生了金的异型叠加成矿作用。
The Jinqingding deposit is in the Mouping rushan gold metallogenic belt.TheJiangjunshi quhezhang fault is the prime ore controling structure in the region whichformed in a multi stage structrural elolution, Different types mineralization have beensuperimpased to one another due to the difference in the structural ore forming periods.
出处
《山东地质》
1995年第1期41-48,共8页
Geology of Shandong
