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新疆萨尔托海豆荚状铬铁矿后期蚀变作用

赵佳玉 申萍 冯浩轩 李昌昊 罗耀清 武阳 楚翔凯 索青宇 白应雄

矿床地质2025,Vol.44Issue(3):559-580,22.
矿床地质2025,Vol.44Issue(3):559-580,22.DOI:10.16111/j.0258-7106.2025.03.003

新疆萨尔托海豆荚状铬铁矿后期蚀变作用

Hydrothermal alteration of Sartohay podiform chromite,Xinjiang

赵佳玉 1申萍 2冯浩轩 3李昌昊 3罗耀清 1武阳 1楚翔凯 1索青宇 1白应雄1

作者信息

  • 1. 中国科学院地质与地球物理研究所岩石圈演化与环境演变全国重点实验室,北京 100029||中国科学院大学地球与行星科学学院,北京 100029
  • 2. 中国科学院地质与地球物理研究所岩石圈演化与环境演变全国重点实验室,北京 100029||中国科学院大学地球与行星科学学院,北京 100029||中国科学院地球科学研究院,北京 100029
  • 3. 中国科学院地质与地球物理研究所岩石圈演化与环境演变全国重点实验室,北京 100029||中国科学院地球科学研究院,北京 100029
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摘要

Abstract

The Sartohay chromite deposit in Xinjiang underwent intense late-stage hydrothermal alteration,resulting in the formation of four types of chromite:① Primary Cr-spinel;② Porous chromite;③ Porous ferrous chromite;④ Homogeneous ferrous chromite.The primary Cr-spinel shows a uniform texture,compositionally belonging to high-Al Cr-spinel.The porous chromite occurs as the irregular metasomatic rims that enclosed the primary Cr-spi-nel,having significantly increased Cr# and decreased Mg# values.The porous ferrous chromite appears as single grains,having higher Cr# values,lower Mg# values,and much higher Fe2+contents than the porous chromite.Ho-mogeneous ferrous chromite,which has the highest Fe3+contents,typically appears as overgrown rims.In the MORB chromite normalized spider diagram,the trace element patterns of the primary chromite spinel are general-ly"flat"with no significant anomalies,while the porous chromite shows obvious depletion of Ni and Sc and slight enrichment of Zn,Co,and Mn.The porous ferrous chromite and homogeneous ferrous chromite are strong-ly enriched in Zn,Co,Mn and Ni,and depleted in Ga and Sc.These textural and compositional features suggest that the primary Cr-spinel has undergone a two-stage fluid-mediated alteration process.In the first stage,the pri-mary Cr-spinel and olivine interact with reducing low-silica fluids to form porous chromite.Subsequently,porous chromite reacted with olivine to produce porous ferrous chromite in the presence of a high-silica-reducing fluid.During the second stage,the porous ferrous chromite interacted with ferrous oxidized fluids to form homoge-neous ferrous chromite under amphibolite facies condition.

关键词

流体/微量元素/变质作用/铬铁矿/萨尔托海

Key words

fluid/trace element/chromite/metamorphism/Sartohay

分类

地质学

引用本文复制引用

赵佳玉,申萍,冯浩轩,李昌昊,罗耀清,武阳,楚翔凯,索青宇,白应雄..新疆萨尔托海豆荚状铬铁矿后期蚀变作用[J].矿床地质,2025,44(3):559-580,22.

基金项目

本文得到自治区重点研发项目(编号:2023B03006)、新疆维吾尔自治区人民政府国家305项目办公室和新疆维吾尔自治区"天池英才"引进计划联合资助 (编号:2023B03006)

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