摘要
斜州地区301地段位于363矿床北西面,距该矿床1.5 km,属363矿床外围。区内印支期和燕山期岩浆活动强烈,地质构造较复杂,多数断裂具有多期次活动的特点,区内构造主要呈北北东-南西西向展布。本文在总结该区的地质特征及控矿构造特征的基础上,对该区铀成矿条件进行了分析。301地段斜州硅化断裂是主要成矿带,成矿条件非常有利,通过勘查有望扩大矿区远景。
Oblique - state area 301 Lot is located in the north west of 363 deposit. 1.5 km from the deposit, is close to external of the 363 deposits. The district has undergone strong Indoian and Yanshanian magmatic activity, geological structure are complicated, multi - period geological structure events, regional structures in this area is north east - south west. based on the geological characteristics and controlling structural character- istics summarizes. This article was analyzed Conditions of uranium mineralization in the area. Lot 301 silicified fracture inclined state is the main ore zone. forming a very favorable conditions. through exploration is expected to expand the mine vision.
出处
《四川建材》
2013年第2期93-94,97,共3页
Sichuan Building Materials
关键词
斜州301地段
地质
构造
成矿分析
Oblique - state 301 Lot
Geological features
Structural Features
metallogenic analyzed
