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长江中下游地区泥盆系-石炭系界面特征分析
引用本文:魏翔,王硕,陈国超,高坡.长江中下游地区泥盆系-石炭系界面特征分析[J].世界地质,2011,30(4):573-578.
作者姓名:魏翔  王硕  陈国超  高坡
作者单位:1. 长安大学地球科学与资源学院,西安710054; 2. 吉林大学地球科学学院,长春130061; 3. 陕西省煤田地质局勘察研究院,西安710054; 4. 湖南有色地质勘察局二四七队,长沙410129
摘    要:长江中下游地区是中国东部重要的铁铜金多金属成矿带。经对比,长江中下游大多数地区的泥盆系五通组与石炭系黄龙组之间有明显的沉积间断,为假整合接触关系。两组岩性差异较大,五通组主要为陆相碎屑沉积,而黄龙组为碳酸盐岩。泥盆系五通组与石炭系黄龙组之间的不整合界面是构造薄弱面,利于成矿元素的聚集,是成矿带内主要的容矿层位,该层位应是今后深部找矿的重要层位。

关 键 词:长江中下游成矿带  五通组  黄龙组  不整合面

Analysis on interface characteristics between Devonian and Carboniferous in middle-lower reaches of Yangtze River
WEI Xiang , WANG Shuo , CHEN Guo-chao , GAO Po.Analysis on interface characteristics between Devonian and Carboniferous in middle-lower reaches of Yangtze River[J].World Geology,2011,30(4):573-578.
Authors:WEI Xiang  WANG Shuo  CHEN Guo-chao  GAO Po
Institution:1. College of Earth Science and Resources,Chang'an University,Xi'an 710054,China; 2. College of Earth Science,Jilin University,Changchun 130061,China; 3. Shanxi Coalfield Geology Bureau Investigation Research Institute,Xi'an 710054,China; 4. 247 Team of Hunan Non-ferrous Geological Exploration Bureau,Changsha 410129,China
Abstract:The metallogenic belt in middle-lower reaches of Yangtze River is a major Fe-Cu-Au polymetallic ore belt in the eastern China. There are significant hiatus between Devonian Wutong Formation and Carboniferous Huanglong Formation, which shows unconformity relationship between the two formations. The two formations are quite different in lithology that the Wutong Formation is mainly of continental elastic sediments, while the Huan- glong Formation is mainly carbonate rocks in nature. The unconformity interface between the two formations is weak in structure, which benefits for the aggregation of metallogenie elements and the major horizon of ore-bearing in the belt, and the horizom is also the key position for deep prospecting in future.
Keywords:middle-lower reaches of Yangtze River  metallogenie belt  Wutong Formation  Huanglong For- mation  unconformity interface
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