辽宁青城子地区印支期岩浆作用与找矿预测

大量研究表明辽宁青城子地区主要成矿作用与印支期岩浆活动有密切关系，为了进一步研究印支期岩浆活动与成矿关系，文章在详细野外工作的基础上，对印支期侵入岩体进行了岩石地球化学测试分析。结果表明，青城子地区印支期花岗岩的w(SiO₂)介于61.67%～77.69%,w(K₂O)介于3.96%～6.67%,w(Na₂O)为0.04%～4.42%，里特曼指数为0.57～5.19，多数小于3.3，主要为高钾钙碱性和钾玄岩系列；在以w(SiO₂)为横坐标、其他氧化物为纵坐标的哈克图解中，除了w(Na₂O)、w(K₂O)与w(SiO₂)的线性关系不明显外，其他氧化物均与w(SiO₂)呈线性关系，说明它们具有明显的岩浆演化关系；微量元素均富集大离子亲石元素，亏损高场强元素，原始地幔标准化配分曲线呈右倾模式，稀土元素球粒陨石标准化配分模式呈轻稀土元素富集、重稀土元素亏损的右倾模式；构造判别图指示了青城子地区印支期岩浆活动产于同碰撞大地...

Indosinian magmatism and ore prospecting prediction in Qingchengzi area, Liaoning Province

A large number of studies have shown that the main mineralization in Qingchengzi area is closely related to the Indosinian magmatism. In order to further study the relationship between magmatic activity and mineralization in Indosinian period, the lithogeochemical analysis of Indosinina intrusive rocks were carried out on the basis of detailed field work. The results show that the SiO₂ content, K₂O content and Na₂O content of Indosinian granites in Qingchengzi area are 61.67%~77.69%, 3.96%~6.67% and 0.04%~4.42%, respectively. The Reitman composite index is 0.57~5.19, mostly less than 3.3, which is mainly high potassium calc-alkaline and shoshonite series. In the Harker diagrams with SiO₂ as the abscissa and other oxides as the ordinate, except Na₂O and K₂O have no obvious linear relationships with SiO₂, other oxides have linear relationship with SiO₂, indicating that they have obvious magmatic evolution relationship. The trace elements are enriched in large ion lithophile elements, depleted in high field strength elements, and the curve of the primitive mantle-normalized shows a right-leaning mode. The pattern of rare earth elements chondrite-normalized shows a right-leaning mode of enrichment of light rare earth elements and depletion of heavy rare earth elements. The tectonic discrimination plots of trace element indicate that the magmatic activity in Qingchengzi area belongs to the syn-collision tectonic environment. According to the geochemical characteristics and the evolution relationship between various rocks, it is determined that their emplacement sequence is the main facies of Shuangdinggou intrusive body→granite porphyry dikes→central facies of Shuangdinggou intrusive body. Through the comparative analysis between the compositions of altered granite porphyry and unaltered granite porphyries, it is considered that granite porphyry can be used as a prospec-ting indicator for lead-zinc and gold-silver deposits. The quantitative distribution density of granite porphyry dikes from a large number of boreholes is highly consistent with the distribution of deposits in the horizontal projection, and it is predicted that the granite porphyry distribution area in the northeast of Taoyuan has great metallogenic potential.