| 秦皇岛柳江盆区地壳演化过程与成矿特征 |
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| 引用本文： | 刘锡文,李连合.秦皇岛柳江盆区地壳演化过程与成矿特征[J].河北理工学院学报,1994(1). |
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| 作者姓名： | 刘锡文 李连合 |
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| 摘 要： | 柳江盆区地壳经过前地槽、地槽、地台和地洼四大不同历史发展阶段，但由于盘内仅发育有地台和地洼两大构造层，因而其成矿作用的大地构造类型只有地合型和地洼型两大类。前者有煤、铝土矿等外生矿产；后者既有外生煤矿，又有内生铅、锌、铜、铁等矿化特征。
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| 关 键 词： | 地壳演化 成矿特征 柳江盆区 秦皇岛 |
CRUSTAL EVOLUTION AND METALLOGENIC CHARACTERS OF THE LIUJIANG DIWA BASIN, QINHUANGDAO |
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| Liu Xiwen, Li Lianhe.CRUSTAL EVOLUTION AND METALLOGENIC CHARACTERS OF THE LIUJIANG DIWA BASIN, QINHUANGDAO[J].Journal of Hebei Institute of Technology,1994(1). |
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| Authors: | Liu Xiwen Li Lianhe |
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| Institution: | Department Of Mining |
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| Abstract: | The Liujiang diwa basin has undergone a development of four periods: Pre-geosyncline,geosyncline,pletform and diwa. Because there are only platform and diwa intural layers in the basin,the metallogenesis is'ouly Platform and diwa-type. The fro mer includes coal bauxife and other exogenetic mineral resources,and the later includes not only ex ogenetic coal but also endogenetic Ph, Zn,Cu and Fe mineralization |
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| Keywords: | Crustal Evolution Metallogenic Character Diwa Basin Liujiang Qinhuangdao |
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