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以往许多学者习惯于将造山作用与造盆作用分开来研究，且认为赣北庐山—鄱阳湖仅在第四纪形成。笔者通过对庐山及其东部鄱阳湖地区区域深部构造背景及其基本地质特征的分析，将庐山—鄱阳湖的造山—造盆作用作为一个整体来进行研究，主要论述了其造山－造盆作用的特征，即先天条件、临产条件和后天条件。在此基础上．将庐山—鄱阳湖的造山—造盆作用划分为前震旦纪基础阶段、震旦纪—早三叠世休眠阶段、晚二叠世—早第三纪雏形阶段及晚第三纪—第四纪形成阶段等四个阶段．并对各阶段造山—造盆作用的运动学与动力学特征进行了探讨。
In the past, many scholars used to study the orogeny and the role of the basin separately, and believed that Lushan-Poyang Lake in northern Jiangxi was formed only in Quaternary. Based on the analysis of the deep tectonic setting and its basic geological features in Lushan and its eastern Poyang Lake region, the author studies the orogenic-sedimentation of Lushan-Poyang Lake as a whole, mainly discusses its orogenicity Characteristics, that is, congenital conditions, labor conditions and acquired conditions. on the basis of. The orogenic-sedimentation of Lushan-Poyang Lake can be divided into the basic stage of Pre-Sinian, the Sinian-Early Triassic dormant stage, the Late Permian-Early Tertiary stage and the Late Tertiary-Quaternary Formation stage and other four stages. The kinematics and dynamics characteristics of orogenic process in each stage are also discussed.