地质与勘探2001，Vol.37Issue(1)：38-43,6.
山东海阳郭城金矿床地质地球化学特征及成因
GEOLOGICAL AND GEOCHEMICAL FEATURES AND GENESIS OF GUOCHENG GOLD DEPOSIT
IN HAIYANG COUNTY, SHANDONG PROVINCE
沈远超 1刘铁兵 1李厚民 1李光明 1刘福涛2
作者信息
- 1. 中国科学院地质与地球物理研究所,
- 2. 中国科学院长春地理研究所,
- 折叠
摘要
Abstract
It is compose of three major mining districts, called Tudui, east Tudui, and Shawang. Authors summarize geological and geochemical features of this gold deposit and discuss its genesis. It is proposed that the gold mineralization was controlled by the combination of contact structure, in terlayer sliding structure, and basic to medium magma activities during the Yans han Period under an extensional tectonic background. The Guocheng gold deposit is one of interlayer sliding fault zone controlled gold deposits along margins of the Mesozoic Laiyang sedimentary basin.关键词
地球化学特征/层间滑动构造/郭城金矿/海阳市分类
天文与地球科学引用本文复制引用
沈远超,刘铁兵,李厚民,李光明,刘福涛..山东海阳郭城金矿床地质地球化学特征及成因[J].地质与勘探,2001,37(1):38-43,6.
