地质找矿论丛2011，Vol.26Issue(4)：373-377,5.
新疆伽师铜矿床地质特征及成因模式
Geological characteristics of Jiashi Cu deposit in Xinjiang and the genetic model
张江1
作者信息
- 1. 中国冶金地质总局新疆地质勘查院,乌鲁木齐 830063
- 折叠
摘要
Abstract
Geological characteristics of Jiashi Cu deposit are discussed and the genetic model is established. Cu ore of the deposit occur conformably in fine paleogene grey white debris-bearing calcareous sandstone as tabular layed bodies. The ore body contacts more sharply with hanging wall due to variation of lithologies in continuous sedimentation and sharply with foot wall due to the common basal sandy, con-glumeritic ore body. The sandy and conglumeritic ore bodies are in wash sedimentary contact. The Cu deposit should be a stratobound Paleogene lake sedimentary sandstone-hosted Cu deposit关键词
伽师铜矿/沉积作用/矿床地质特征/砂岩铜矿/成因模式/新疆Key words
Jiashi Cu deposit/ sedimentation/ characteristics of the deposit/ sandstone-hosted Cu deposit/ genetic model/ Xinjiang分类
天文与地球科学引用本文复制引用
张江..新疆伽师铜矿床地质特征及成因模式[J].地质找矿论丛,2011,26(4):373-377,5.
