| 陈旺.豫西济源西部铝土矿成矿地质环境[J].地质与勘探,2007,(1):26-31 |
| 豫西济源西部铝土矿成矿地质环境 |
| ORE -FORMING CONDITIONS OF BAUXITE DEPOSITS IN WESTERN JIYUAN, HENAN |
| 修订日期：2005-12-14 |
| DOI： |
| 中文关键词: 济源西部 铝土矿 古地理环境 |
| 英文关键词: western Jiyuan, bauxite deposit, palaeogeographical environment |
| 基金项目: |
| 陈旺 |
| [1]中国地质大学,北京100083 [2]河南省有色金属地质勘查总院,郑州450052 |
| 摘要点击次数: 1954 |
| 全文下载次数: 1447 |
| 中文摘要: |
| 文章在对含矿岩系岩石组合、地球化学分析的基础上,认为矿区铝土矿形成于华北地块从早古生代准平原状态向晚古生代陆表浅海过渡时期,早期海侵之后的陆地湖泊环境中.被碳酸盐岩覆盖、较小地形差异的陆地准平原状态,湿热的气候,繁茂的植物使得岩溶湖泊成为铝土矿富集和保存的有利场所. |
| 英文摘要: |
| Based on studies of ore - bearing rocks and geochemistry, it is suggested that bauxite deposits in western Jiyuan were sediments in lake - environments after transgression when North China Block turned from peneplain in early Paleozoic to epeiric sea in late Paleozoic. Land covered by limestone, peneplain, humid climate, and flourish plants made karst lakes the best places for enriching and preservation of bauxite. The area covered by Permian strata in the northeast parts is good for prospecting. |
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