| 简析陈家堡子白云岩矿床成矿地质特征 |
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| 引用本文： | 范永红. 简析陈家堡子白云岩矿床成矿地质特征[J]. 有色矿冶, 2021, 0(2): 1-3,18 |
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| 作者姓名： | 范永红 |
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| 作者单位： | 辽宁省有色地质一○七队有限责任公司 |
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| 摘 要： | 陈家堡子白云岩矿床产于辽河群中部以及下部碳酸盐岩中,其原岩建造应属浅海相化学沉积碳酸盐岩建造,经过区域变质作用,在一定的温度和压力下发生重结晶,局部含镁质热液富集交代形成白云岩矿.
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| 关 键 词： | 沉积碳酸盐 区域变质 白云岩矿床 |
A Brief Analysis of Metallogenic Geological Characteristics of the Chenjiapuzi Dolomite Deposit |
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| FAN Yong-hong. A Brief Analysis of Metallogenic Geological Characteristics of the Chenjiapuzi Dolomite Deposit[J]. Non-Ferrous Mining and Metallurgy, 2021, 0(2): 1-3,18 |
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| Authors: | FAN Yong-hong |
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| Affiliation: | (Liaoning Province Nonferrous Geological team 107 Co.,Ltd.,Dalian 116113,China) |
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| Abstract: | The Chenjiapuzi dolomite deposit occurs in the central and lower carbonate rocks of Liaohe group,the original rock formation belongs to neritic facies chemical sedimentary carbonate rock formation,through regional metamorphism,recrystallization occurs under certain temperature and pressure,and local magnesium-bearing hydrothermal metasomatism is enriched to form dolomite ore. |
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| Keywords: | sedimentary carbonate regional metamorphism dolomite deposit |
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