埃及西奈阿布泽尼玛地区铀矿成矿地质特征及控制因素分析  

Uranium Metallogeny and Ore Controlling Factor in Abu Zenima District,Sinai,Egypt

作　　者：张运涛[1,2] 裴荣富[1] 张小平 曾文乐 王浩琳[1] 黄符桢 邵长亮[4] 

机构地区：[1]中国地质科学院矿产资源研究所,北京100037 [2]江西省核工业地质局二六四大队,江西赣州341000 [3]江西省核工业地质局,江西南昌330046 [4]天津华北地质勘探局,天津300171

出　　处：《东华理工大学学报（自然科学版）》2010年第4期339-344,共6页Journal of East China University of Technology(Natural Science)

摘　　要：埃及西奈半岛盛产铁锰矿、铜矿、铀矿、高岭石、石英砂等矿产,铀与铜、铁锰矿有一定的空间联系。笔者通过在阿布泽尼玛成矿区多年的工作实践和研究,对该区铀成矿地质特征进行了分析,圈定了7个铀矿赋矿层位,总结了该区铀矿化分布规律,获得了同生沉积、后生叠加改造的成因认识。The Sinai Peninsula is well-known with ferromanganese,copper,uranium,kaolinite and quartz sands and etc.in Egypt.Among them,uranium mineralization is closely related with copper and ferromanganese in space.Based on detailed field investigation and study in metallogenetic region in Abu Zenima district,uranium metallogeny has been analyzed,7 uranium host strata are delineated and uranium distribution regularity has been summarized.Syngenetic sedimentation but epigenetic superimposed and transformed metallogeneses are concluded.

关 键 词：阿布泽尼玛地区 铀矿化 分布规律 赋矿层位 

分 类 号：P619.14[天文地球—矿床学]