鄂西“神农架式铁矿”地质特征及找矿方向  

PROSPECTING DIRECTIONS AND GEOLOGICAL CHARACTERISTICS OF 'THE SHENNONGJIA TYPE IRON DEPOSIT' IN WESTERN HUBEI

作　　者：蔡雄威[1] 

机构地区：[1]中南冶金地质研究所,湖北宜昌443003

出　　处：《资源环境与工程》2006年第5期509-512,547,共5页Resources Environment & Engineering

摘　　要：神农架地区是湖北省境内重要的成矿区之一。区内的铁矿主要为浅海沉积型赤铁矿,被称为“神农架式铁矿”。通过对区内该类铁矿的地质特征及控矿地质因素分析,阐述区内该类矿床在含矿建造、控矿层位、控矿岩性、控矿岩相以及构造控矿等方面的特点,从而为区内地质找矿指明方向。The Shennongjia is one of important ore-formation areas in the west of Hubei Province. The deposit called ＇ Shennongjia type iron deposit＇ occurs mainly as the shallow sea sedimentary hematite deposit. The author analyzes its geological characteristics and the ore-control factors, discusses its features such as iron-bearing formations ,ore-control horizon , facies,and structures. The author also points out the directions for further iron exploration in the area.

关 键 词：神衣架式铁矿 地质特征 控矿因素 找矿方向 

分 类 号：P618.31[天文地球—矿床学] P611[天文地球—地质学]