摘要
本文主要讨论了赣杭构造带中生代火山盆地形成和演化的基本模式;论述了盆地内外两侧截然不同的演化规律,坳陷、断陷、塌陷式火山盆地与火山穹窿等火山构造的相互关系,火山盆地盖层间破碎带的形成及与火山盆地演化的关系等。
This paper mainly discusses the principle model for the formation and the evolution of Mesozoic volcanic basins in the Gan Hang Tectonic Belt, and describes the distinct evolution features between the internal and external sites of volcanic basins, the natural relation between the down warped, down faulted, collapse volcanic basins and volcanic domes, the relationship between the formation of interlayered fractured zones of the volcanic cover and the evolution of volcanic basins.
出处
《铀矿地质》
CAS
CSCD
1999年第1期18-23,共6页
Uranium Geology
关键词
赣杭构造带
火山盆地
层间破碎带
盆地
铀矿床
Gan Hang Tectonic Belt, Volcanic basin, Interlayered fractured zone