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内蒙古千里山铁矿成矿地质特征及矿物学研究

张燕 皮桥辉 余胜

山东国土资源2026,Vol.42Issue(1):26-38,13.
山东国土资源2026,Vol.42Issue(1):26-38,13.DOI:10.12128/j.issn.1672-6979.2026.01.004

内蒙古千里山铁矿成矿地质特征及矿物学研究

Study on Ore-forming Geological Characteristics and Mineralogy of Qianlishan Iron Deposit in Inner Mongolia

张燕 1皮桥辉 1余胜1

作者信息

  • 1. 桂林理工大学地球科学学院,广西 桂林 541006
  • 折叠

摘要

Abstract

In this paper,geological characteristics of Qianlishan study area located within early Proterozoic Khondalite Belt in the western block of the North China Craton have been studied.Qianlishan iron deposit is located in Wuhai city in Inner Mongolia with complex geological structures.Through analyzing petro-graphic characteristics in this area,diopside-mica-scapolite schist,hornblende Monzonite gneiss and di-opside-biotite-scapolite-hornblende schist have been identified.According to electron probe microanaly-sis(EPMA)results,it is indicated that Qianlishan hornblende is mostly of high-grade metamorphic ori-gin.It has reflected the characteristics of ancient basement and abundant metamorphic rock.The biotite is mantle-derived,and near the crust mantle mixed source.It is favorable for mineralization of Au,Mo,Cu,and Fe.The chemical composition of pyroxene shows that the parent magma belongs to the tholeiitic series,characterized by high SiO2,low TiO2,Al2O3 and Na2 O.In addition,high crystallization tempera-tures of pyroxene and biotite in Qianli Mountain area indicate high-temperature characteristics of parent magma.High oxygen fugacity biotite may indicate good mineralization potential for Fe,Cu,and Au.This study provides important clues for mineral exploration.

关键词

矿物成分分析/变质成因/温压条件/千里山铁矿/内蒙古

Key words

Mineral composition analysis/metamorphic origin/temperature and pressure conditions/Qian-lishan iron deposit/Inner Mongolia

分类

天文与地球科学

引用本文复制引用

张燕,皮桥辉,余胜..内蒙古千里山铁矿成矿地质特征及矿物学研究[J].山东国土资源,2026,42(1):26-38,13.

基金项目

广西自然科学基金面上项目:锡在富F还原性热液体系中成矿过程的实验和计算模拟研究(项目编号:2022JJA150094) (项目编号:2022JJA150094)

山东国土资源

1672-6979

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