首页> 外文期刊>Russian journal of Pacific geology >Specific features of the fluid regime during the formation of systems with copper-molybdenum-gold and copper-tin mineralizations (Iskra-Soboliny knot, Kavalerovo ore district, Primorye)
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Specific features of the fluid regime during the formation of systems with copper-molybdenum-gold and copper-tin mineralizations (Iskra-Soboliny knot, Kavalerovo ore district, Primorye)

机译:铜-钼-金和铜-锡矿化系统形成过程中流体状态的特殊特征(Iskra-Soboliny结,Kavalerovo矿区,滨海边疆区)

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摘要

Specific features of the fluid regime in ore-magmatic systems located in the southwestern part of the Kavalerovo ore district (Primorye) are considered. One system is accompanied by mineralization of the porphyry copper type (Lazurnoe deposit); the other system, by tin (copper-tin) mineralization of the hydrothermal type (Iskra deposit). It is shown that the magmatic stages of these systems are distinguished mainly by the chlorophile nature of the copper-gold system and the fluorophile nature of the copper-tin system. The well-known distinction of these systems in terms of the redox parameter is confirmed, and its different evolution scenarios in the systems are shown. The results of the study of fluid inclusions in quartz of postmagmatic associations show that the processes of ore formation at the Lazurnoe deposit were characterized by a wide temperature range and the heterogeneity of the mineral-forming environment. The early period was marked by the coexistence of aqueous-saline brines (mainly of Na-Ca-Mg-chloride composition) and low-density fluid inclusions. The late period was dominated by ordinary hydrothermal solutions. The Iskra deposit formed in a relatively narrow temperature range from homogeneous fluids of essentially Na-chloride composition characterized by moderate and low salinity.
机译:考虑了位于卡瓦列罗沃矿区(Primorye)西南部的矿石-岩浆系统中流体状态的特定特征。一种系统伴随着斑岩型铜矿(Lazurnoe矿床)的矿化;另一个系统是通过水热型锡(铜锡)矿化(伊斯克拉矿床)。结果表明,这些系统的岩浆阶段主要以铜金系统的亲氯性质和铜锡系统的亲氟性质为特征。确认了这些系统在氧化还原参数方面的众所周知的区别,并显示了其在系统中的不同演变情况。后岩浆化合石英中流体包裹体的研究结果表明,Lazurnoe矿床的成矿过程具有较宽的温度范围和成矿环境的非均质性。早期的特点是盐水和盐水(主要是氯化钠-钙-镁氯化物)和低密度流体包裹体并存。后期主要是普通的水热溶液。 Iskra沉积物是在相对较窄的温度范围内由特征在于中等盐度和低盐度的基本氯化钠组成的均质流体形成的。

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