| 保山核桃坪铅锌多金属矿矿化特征新认识 |
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| 引用本文： | 姜龙燕.保山核桃坪铅锌多金属矿矿化特征新认识[J].云南地质,2011,30(1):38-41. |
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| 作者姓名： | 姜龙燕 |
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| 作者单位： | 香港悦达矿业公司,云南,昆明,653100 |
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| 摘 要： | 保山核桃坪铅锌矿可划分14个矿带、33支矿床。矿体均受断层或裂隙控制，主矿化方向有四组，成矿规律有差异。北北西向矿化最强，为核桃坪矿区主矿体，近矿围岩蚀变中矽卡岩化最重要，分为简单和复杂两类，尤以复杂矽卡岩化为重要。
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| 关 键 词： | 铜铅锌多金属 分带分层 近矿围岩蚀变 岩性构造控矿 云南保山核桃坪 |
THE NEW COGNITION OF METALLOGENESIS CHARACTERISTICS OF HETAOPING PB-ZN MULTIMETALLIC DEPOSIT IN BAOSHAN |
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| JIANG Long-yan.THE NEW COGNITION OF METALLOGENESIS CHARACTERISTICS OF HETAOPING PB-ZN MULTIMETALLIC DEPOSIT IN BAOSHAN[J].Yunnan Geology,2011,30(1):38-41. |
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| Authors: | JIANG Long-yan |
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| Institution: | JIANG Long-yan(Yueda Mining Company Limited of Hongkong,Kunming 653100) |
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| Abstract: | The ore bodies of Hetaoping Pb-Zn deposit are controlled by the fault or fissure.There are 4 sets of main metallogenesis direction.The metallogenesis rule is different.The metallogenesis of NNW direction is the most intense,which forms the main ore body in Hetaoping Orefield.The important wall rock alteration near the ore body is the skarn,which can be divided into the simple and complicated type.And the complicated skarn is the important one. |
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| Keywords: | Cu-Pb-Zn Multimetallic Deposit Division of Zone and Horizon Wall Rock Alteration near Ore Body Ore Control of Rock and Structure Hetaoping Baoshan Yunnan |
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