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期刊界 All Journals 搜尽天下杂志传播学术成果专业期刊搜索期刊信息化学术搜索

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

引用本文：	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,1991,6(2):71-82.

作者姓名：	刘斌

作者单位：	同济大学地下建筑与工程系

摘要：
关键词：	火山岩海相铁矿带流体包裹体
CHARACTERISTICS OF THE FLUID INCLUSIONS AND THERMALDYNAMIC CONDITIONS OF MINERALIZATIONS IN THR IRON ORE BELT OF MARINE VOLCANIC ROCKS,ALTAI,XINJIANG

Liu Bin.CHARACTERISTICS OF THE FLUID INCLUSIONS AND THERMALDYNAMIC CONDITIONS OF MINERALIZATIONS IN THR IRON ORE BELT OF MARINE VOLCANIC ROCKS,ALTAI,XINJIANG[J].Contributions to Geology and Mineral Resources Research,1991,6(2):71-82.

Authors:	Liu Bin

Affiliation:	Department of Underground Building and Engineering, Tongji University, Shanghai

Abstract:	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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