雷鸣盆地地质构造特征及盆地演化  

Characteristics of geological structure and basin evolution in the thunder Basin

作　　者：陈华祝 黄伟 许丽丽 CHEN Hua-zhu;HUANG Wei;XU Li-li(Hainan Nuclear Industry Geological Brigade,Haikou 571100,China;29 Research Institute of nuclear industry,Shaoguan 512000,China)

机构地区：[1]海南省核工业地质大队,海南海口571100 [2]核工业二九〇研究所,广东韶关512000

出　　处：《世界有色金属》2018年第14期212-213,共2页World Nonferrous Metals

摘　　要：本文根据盆地区域地层分布特征,以及地质构造特征,分析盆地形成时代,研究盆地构造演化历史,总结认为雷鸣盆地的形成受构造、古地理作用控制,发育不同时期的沉积建造,变质建造和构造相,具有多旋回的地质演化发展特征。According to the regional stratigraphic distribution and geological structure characteristics of the basin, this paper analyzes the formation age of the basin, studies the tectonic evolution history of the basin, and concludes that the formation of the Leiming basin is controlled by tectonics and palaeogeography, develops sedimentary formation, metamorphic formation and tectonic facies in different periods, and has a multi-cycle geology. Characteristics of evolution and development.

关 键 词：雷鸣盆地 构造特征 鹿母湾组 报万组 演化 

分 类 号：P618.13[天文地球—矿床学]