| 刘斌.新疆阿勒泰海相火山岩铁矿带中流体包裹体特征和成矿作用的热力学条件[J].地质找矿论丛,1991,(2):71-82 |
| 新疆阿勒泰海相火山岩铁矿带中流体包裹体特征和成矿作用的热力学条件 |
| CHARACTERISTICS OF THE FLUID INCLUSIONS AND THERMALDYNAMIC CONDITIONS OF MINERALIZATIONS IN THR IRON ORE BELT OF MARINE VOLCANIC ROCKS,ALTAI,XINJIANG |
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| DOI：10.6053/j.issn.1001-1412.1991.2. 007 |
| 中文关键词: 海相火山岩 铁矿带 流体包裹体 热力学条件 |
| 英文关键词: |
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| 摘要点击次数: 1018 |
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| 中文摘要: |
| 由海相火山岩铁矿带划分的五个成矿作用阶段,进行矿物流体包裹体的系统研究。阐述了四种类型的流体包裹体在不同成矿阶段中的分布特征。计算出不同阶段成矿溶液的热力学条件:温度、压力、氧逸度、流体成分、密度、含盐度。对该成矿带铁质来源、成矿方式、矿床成因进行了探讨。从而、初步建立了本矿带成矿模式。 |
| 英文摘要: |
| Five mineralization stages can be recognized in the iron ore deposits in the Altai Area, Xinjiang.Sampes are systematically collected from the stages for inclusion study (temperature, pressure, fo2,composition, density, salinity, etc).Based on the analysis and calculations the source of iron and the genesis of the deposits are determined and a metallogenic model is established. |
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