作　　者： (陈雷超）; (胡金苗）;

机构地区： 成都理工大学地球科学学院,四川成都610059

出　　处： 《云南化工》 2017年第8期119-120,共2页

摘　　要： 赣南中生代盆地的沉积源于早白垩世,以拗陷为主。控盆构造主要为洞口一合龙北东向同沉积断裂,该断裂属赣江断裂系万安一乐安深大断裂的一部分。对盆地的形态,深部地球物理特征,沉积特征及控盆因素调查研究,并结合区域资料解析白垩纪晚世盆地构造及演化规律。 The sedimentary origin of the Mesozoic basin originated from early cretaceous and was dominated by depression.The control basin is mainly formed by the north east and the same sedimentary faults in the north east of the cave.This paper studies the morphology, geophysical characteristics, sedimentary characteristics and control basin factors of the basin, and analyzes the structure and evolution of late cretaceous in conjunction with regional data.

关 键 词： 沉积盆地 白垩纪 同沉积断裂 继承性