| 凤太矿田层控铅锌(铜)矿床的成矿物质来源探讨 |
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| 引用本文： | 隗合明,吕仁生. 凤太矿田层控铅锌(铜)矿床的成矿物质来源探讨[J]. 地球科学与环境学报, 1990, 0(1) |
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| 作者姓名： | 隗合明 吕仁生 |
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| 作者单位： | 西安地质学院地勘系(隗合明)，西安地质学院地勘系(吕仁生) |
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| 摘 要： | 秦岭凤太矿田层控铅锌(铜)矿床的金属物质、硫和成矿溶液主要来自深部基底的岩石,属海底喷流—沉积成因矿床。从这一理论认识出发可进一步分析控矿地质条件及今后在该区有效地寻找同类矿床。
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| 关 键 词： | 凤太矿田 成矿物质来源 同生热液 海底喷流—沉积矿床 |
AN EXPLORATORY STUDY OF THE SOURCE OFMINERALIZED MATERIALS IN THE STRATABOUNDPb-Zn- ( Cu ) ORE DEPOSITS OF THE FENGTAI OREFIELD IN THE QINLING MOUNTAINS |
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| Wei Heming and Lu Rensheng. AN EXPLORATORY STUDY OF THE SOURCE OFMINERALIZED MATERIALS IN THE STRATABOUNDPb-Zn- ( Cu ) ORE DEPOSITS OF THE FENGTAI OREFIELD IN THE QINLING MOUNTAINS[J]. Journal of Earth Sciences and Environment, 1990, 0(1) |
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| Authors: | Wei Heming and Lu Rensheng |
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| Affiliation: | Xi' an College of Geology |
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| Abstract: | |
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| Keywords: | Fengtai ore field minerogenetic material source syngenetic hydrothermal solution sea-floor exhalation sedimentary meneral deposit |
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