在绘制第 1000/3 号国家地质图时确定斑岩型钼铜矿化的新前景:以 O-55 和 O-56 号图幅(马加丹州普里奥霍特耶北部)为例

Antonina Alenicheva, Nikita Kasatkin, Yuri Yurchenko, Tatyana Zubova, Vitali Shatov, Sergei Sergeev
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引用次数: 0

摘要

根据绘制国家地质图 1000/3,O-55、O-56 号图幅的结果,在马加丹地区发现了莫季克利斯基、奇斯托泽尼和帕夫洛维奇斯基新矿群,这些矿群有望形成斑岩型钼铜矿化。斑岩型矿化与普里奥霍茨基(Priokhotsky)岩浆岩带有关,该岩浆岩带由钙质-碱性系列(K/Na <1)的马加丹岩套阿尔卑斯-前一世纪花岗岩组成。这些花岗岩主要由斑状英安岩和 I 型磁铁矿系列的石英闪长岩组成,成分通常为赤铁矿。矿化由侏罗纪-下白垩统岛弧沉积火山岩地层容纳。U-Pb SIMS SHRIMP 和 Re-Os TIMS 测定证实了矿化与花岗岩之间的关系。在潜在的矿群中,矿化表现为广泛的热液-金属蚀变(丙铁矿和石英-闪锌矿-黄铁矿变质岩)。建议在潜在矿群区域进行后续大规模地质调查和勘探。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Identification of new objects promising for porphyry molybdenum-copper mineralization when creating the State geological map 1000/3: Sheets O-55, O-56 (Northern Priokhotye, Magadan region) as an example
The Motykleisky, Chistoozerny, and Pavlovichsky new ore clusters promising for porphyry molybdenum-copper mineralization have been identified in the Magadan region due to results of creation of the State Geological Map 1000/3, sheets O-55, O-56. The porphyry-type mineralization is associated with the Priokhotsky plutonic belt of Albian-Cenomanian granitoids of the Magadan suite of the calcareous-alkaline series (K/Na <1). The granitoids are dominated by porphyritic tonalites and quartz diorites of type I magnetite series, often adakitic in composition. The mineralization is accommodated by the Jurassic-Lower Cretaceous island-arc sedimentary-volcanic formations. Relationship between the mineralization and granitoids is substantiated by the U-Pb SIMS SHRIMP and Re-Os TIMS dating. In potential ore clusters, the mineralization is manifested by extensive fi lds of hydrothermal-metasomatic alterations (propylites and quartz-sericite-pyrite metasomatites). Recommendations are given for follow-up large-scale geological survey and prospecting in the area of the potential ore clusters.
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