| 吉林基性超基性岩的地质特征及找矿方向 |
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| 引用本文： | 冯守忠,路瑞春.吉林基性超基性岩的地质特征及找矿方向[J].矿产与地质,1992,6(3):183-187. |
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| 作者姓名： | 冯守忠 路瑞春 |
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| 作者单位： | 中国有色金属工业总公司吉林矿产地质研究所 长春130012
(冯守忠)，中国有色金属工业总公司吉林矿产地质研究所 长春130012(路瑞春) |
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| 摘 要： | 从多旋回大地构造演化的观点,分析吉林区域多旋回的构造运动,控制多旋回的基性超基性岩浆活动及其相应的成矿作用,认为与含镍有关的基性超基性岩体,主要受“台槽边界”赤峰—开源深断裂控制,沿深断裂一侧或两侧成带分布,分群集中。为铜镍矿床区域勘查工作,提供地质资料。
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| 关 键 词： | 基性超基性 铜矿 镍矿 找矿 岩型 |
GEOLOGICAL FEATURES OF BASIC-ULTRABASIC ROCKS AND ITS PROSPECTING DIRECTION IN JILIN PROVINCE |
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| Feng Shouzhong Lu Ruichun.GEOLOGICAL FEATURES OF BASIC-ULTRABASIC ROCKS AND ITS PROSPECTING DIRECTION IN JILIN PROVINCE[J].Mineral Resources and Geology,1992,6(3):183-187. |
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| Authors: | Feng Shouzhong Lu Ruichun |
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| Abstract: | From the point of view on polycyclic geotectonic evolution ,the regional polycyclic tectonization in Jilin province controlling both of basic -ultrabasic magmatic activity and corresponding mineralization was discussed. It is suggested that the nickeliferous basic-ultrabasic rock-masses are mainly controlled by Chifeng-Kaiyuan depth fault between platform and geosyncline boundary ,and are zanally distributed and concentrated in groups along one or both sides of the depth fault,providing geological data for the regional prospecting of Cu - Ni ore deoposit. |
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| Keywords: | Polycyclic tectonization Basic -ultrabasic rocks Cu - Ni ore Deposit |
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