Many scientists used to study orogenesis and basinogenesis separately, and thought that the Lushan Mountain-Poyang Lake, North Jiangxi province, only formed in the Quaternary. On the basis of analysis of the regional deep-tectonic setting and main geological characteristics, the orogenesis-basinogenesis in the Lushan Mountain-Poyang Lake as a whole was studied, and its congenital, parturient and postnatal conditions were mainly discussed. On the above basis, four stages of orogeneis -basinogenesis in the Lushan Mountain -Poyang Lake were recognized: the presinian basic, the Sinian-Early Permain dormant, the Late Permain-Early Tertiary embryonic and the Late Tertiary-Quaternary forming stage, and the kinematic-dynamic characteristics of orogenesis-basinogenesis at each stage were discussed.
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