| 中国北方超大型热水沉积硫化物矿床成矿模式 |
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| 引用本文： | 李英,祁思敬.中国北方超大型热水沉积硫化物矿床成矿模式[J].矿物岩石地球化学通报,1997(3). |
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| 作者姓名： | 李英 祁思敬 |
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| 作者单位： | 西安地质学院 |
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| 摘 要： | 中国北方超大型热水沉积硫化物矿床成矿模式李英祁思敬（西安地质学院，西安７１００５４）关键词超大型矿床热水沉积作用大陆边缘盆地热旋回中国北方超大型热水沉积硫化物矿床（ＳＥＤＥＸ）集中产出于华北地台北缘西段与扬子地台北缘西段，即秦岭与狼山两区。可确定的矿...
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| 关 键 词： | 超大型矿床 热水沉积作用 大陆边缘盆地 热旋回 |
Metallogenic Model for Super Large Type Sedimentary hydrothermal (SEDEX) Sulfide Ore Deposits in North China |
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| Li Ying,Qi Sijing.Metallogenic Model for Super Large Type Sedimentary hydrothermal (SEDEX) Sulfide Ore Deposits in North China[J].Bulletin of Mineralogy Petrology and Geochemistry,1997(3). |
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| Authors: | Li Ying Qi Sijing |
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| Abstract: | There are two major metallogenic provinces of super large sedimentary hydrothermal sulfide ore deposits in North China:Langshan mountains and Qinling range,such as Changba Zn Pb deposits, Dongshengmiao Zn pyrite deposits et al Those ore deposits were formed by the hydrothermal convection system circulating through underlying sedimentary columns and the basement in the progressive heating stages of the thermal cycle during the transformation periods from tension to compression of the non active continental margins |
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| Keywords: | super large type sedimentary hydrothermal process continental margin basin thermal cycle |
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