摘要
本文对庐枞地区主要含矿层位、岩浆岩的特点及演化规律、区域构造特征及长江构造带的组成与形成等提出了新认识。有利层位、扬子式壳－幔混熔型岩浆岩成岩系列、区域性深大断裂及其次级构造的活动，为本区铀和多金属矿产的形成，提供了良好的区域地质背景。
This paper presents a new understanding of features of main ore-bearing horizons and magmatic rocks, evolutional regularities, regional tectonic characteristics and the compositions and formation of the Yangtze tectonic belt in Lu-Zong region. Favourable horizons,magmatic series of Yangtze-type crust-mantle mixed melting magmatic rocks,activities of regional gigantic deep-seated faults and their subsidiary structures provided good regional geological setting for the formation of uranium and polymetallic mineral resources in this region.
出处
《铀矿地质》
CSCD
北大核心
1996年第2期75-82,共8页
Uranium Geology
关键词
铀矿床
成矿
区域地质
地质背景
Ore-hosting horizon
Mixed-melting type magmatic rock
Fault structure
