| 福建大田琴山铁矿地质特征及成因初探 |
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| 引用本文： | 林喜.福建大田琴山铁矿地质特征及成因初探[J].福建地质,2011,30(2):101-107. |
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| 作者姓名： | 林喜 |
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| 作者单位： | 福建省地质调查研究院,福州,350013 |
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| 基金项目： | 本文是在大田琴山铁矿详查工作的基础上,根据矿区资料编写而成,感谢项目组同事黄新鹏工程师、林文成工程师大力支持.在成文过程中得到刘贤恩高级工程师的热情指导,并承蒙傅树超教授级高级工程师、刘乃忠高级工程师审阅,一并提出了宝贵的修改意见,在此深表谢意! |
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| 摘 要： | 大田琴山铁矿主矿体呈似层状贮存于晚古生代经畲组中,其形态和产状受地层控制明显,次要矿体以脉状、透镜状居多;岩浆期后热液叠加、改造显著,属沉积-热液改造型矿床.
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| 关 键 词： | 铁矿 地质特征 沉积-热液改造型 大田琴山 |
Peliminary Study of the Genesis and the Geologic Characteristics of the Qingshan Iron Ore in Datian County, Fujian Province |
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| Lin Xi.Peliminary Study of the Genesis and the Geologic Characteristics of the Qingshan Iron Ore in Datian County, Fujian Province[J].Geology of Fujian,2011,30(2):101-107. |
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| Authors: | Lin Xi |
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| Institution: | Lin Xi(Fujian Institute of Geology Survey and Research,Fuzhou,350013) |
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| Abstract: | The ore bodies of the Qingshan iron are stratiform and occur in the late paleozoic Jingshe formation,and form and occurrence are evidently controlled by the layer.The secondary orebody mostly acts like a veiny and lenticular.It is remarkably transformated the postmagmatic hydrothermal superimposed.It belongs to the deposit of the sedimentary-hydrothermal reforming type. |
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| Keywords: | iron ore geologic characteristics sedimentary-hydrothermal reforming type Qingshan area of Datian County |
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