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《Mineral Deposits》 2011-04
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Metamorphic chronology of the BIF in Malanzhuang of eastern Hebei Province and its geological implications

LI YanHe1,2,ZHANG ZengJie1,2,WU JiaShan3 and SHANG LongPing4(1 MLR Key Laboratory of Metallogeny and Mineral Assessment,Institute of Mineral Resources,CAGS,Beijing 100037,China;2 Key Laboratory of Isotope Geology of Ministry of Land and Resources,Beijing 100037,China;3 Institute of Geology,CAGS,Bei-jing 100037,China;4 Beijing Institute of Exploration Techniques,Beijing 100085,China)  
The Precambrian Banded Iron Formations(BIF) are the most important iron resource both in China and abroad,whether in the exploratory reserves or in the quantity of the exploitation.BIF were also the special geochemical sediments in the early earth history which recorded the composition and the redoxomorphic stage of the contemporary atmosphere and the ocean as well as their evolution.The paleo-weathering crust of BIF,which is the most enriched iron ore,is widely distributed in the world.However,this type of BIF has never been found in China.Why is the paleo-weathering crust of BIF absent in China? This is the main focus of this paper.The authors investigated the metamorphic chronology of the BIF in Malanzhuang by means of SHRIPMP II analysis of the zircons from the granitic rocks which occur in the interlayer of the BIF.Based on a comparative study of the time of the BIF formation,the authors have concluded that the BIF in China were deeply buried immediately after their formation,and subsequently they experienced regional metamorphism and migmatization.The BIF in China experienced no weathering for a long time at the earth's surface,which is the reason why the paleo-weathering crust type of enriched iron ore cannot be found in China.
【Fund】: 国家自然科学基金(项目编号:40273008 40203003);; 公益行业科研专项(项目编号:201111002);; 地质调查项目(项目编号:1212010916067)的联合资助
【CateGory Index】: P618.31
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