江西省新余铁矿田区域成矿控矿地质条件与找矿思路
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摘要
新余铁矿田是江西最主要的钢铁原料基地,本文在综合分析良山铁矿地质特征的基础上,分析研究新余铁矿田区域成矿规律及控矿地质条件,提出了主攻已知矿区外围及深部,开辟赋矿向形(斜)构造勘查区,重新查证神山背斜北侧北磁异常带的找矿思路。
The Xinyu iron ore field is the main base of Steel raw material in Jiangxi province.based on the comprehensive analysis of geological characteristics of Liangshan iron ore,the regional metallogenic regularity and ore-controlling geological conditions of Xinyu iron ore field was analysised and researched,and the prospecting ideas that studing the peripheral and deep part of known mine mainly and opening up the hosting synform as the Structure exploration area and to verify the magnetic anomaly belt in the north of Shenshan anticline was put forward.
The Xinyu iron ore field is the main base of Steel raw material in Jiangxi province.based on the comprehensive analysis of geological characteristics of Liangshan iron ore,the regional metallogenic regularity and ore-controlling geological conditions of Xinyu iron ore field was analysised and researched,and the prospecting ideas that studing the peripheral and deep part of known mine mainly and opening up the hosting synform as the Structure exploration area and to verify the magnetic anomaly belt in the north of Shenshan anticline was put forward.
引文
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[2]杨明桂,等.江西北部金属成矿地质[M].北京:中国大地出版社,2004,7:1-29.
[3]江西地质科学研究所.江西省铁矿地质特征分布规律与找矿方向[R].1981,8.
[4]汤加富,朱家安.江西省铁矿地质持征分布规律与找矿方向[M].南昌:江西地质科学研究所,1980,42-108.
[5]汤加富,符鹤琴,余志庆.华南晚前寒武纪硅铁建造的层位、类型与形成条件[J].矿床地质,1987,6(1):1-10.
[6]许温复,王仁根.赣中新余式变质铁矿勘查过程中的小构造研究[J].江西地质科技动态,1958,18-29.
[7]余志庆,汤家富,符鹤琴."新余式"铁矿地质特征及其成因[J].矿床地质,1989,8(4):1-10.
[8]江西地质矿产局.江西省区域地质志[M].北京:地质出版社,1984,766-767.
[9]江西地矿厅.江西岩石地层[M].北京:地质出版社,1997,20-90.
[10]周建廷,王学平,刘川.新余铁矿田中的地质系统律和地质全息律[J].东华理工大学学报,2009,3(30):211-216.
[11]曾书明,周建廷,王学平,等.江西新余铁矿田铁矿成矿地质特征与成因分析[J].地质与勘探,2011,2:187-195.
[12]沈保丰,等.中国前寒武纪成矿作用.北京:地质出版社,2006.1,21-71,275-281.
[13]地质部江西省地质局区域地质调查大队.江西省震旦系[R].1983.
[14]江西省地质矿产局.江西省区域地质特征、成矿条件及成矿规律.江西省区域矿产总结[R].1989.
[15]江西省地质矿产局.江西省区域地质志[M].北京:地质出版社,1994,706-805.