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《Acta Geological Sinica》 1992-04
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SEDIMENTARY CHARACTERISTICS OF THE CRETACEOUS SONGLIAO BASIN

Liu Zhaojun, Wang Dongpo, Liu Li, Liu Wanzhu, Wang Pujun, Du Xiaodi and Yang Guang (Changchun College of Geology, Changchun, Jilin)  
The Songliao basin is a Mesozoic continental rift basin. The rupture of the lithosphere in the Late Jurassic brought about the eruption of basaltic magma. The evolution of the basin progressed through 6 stages: pre-rift doming, extensional fractering, fault subsidence, fault downwarping, downwarping and shringkage, rensulting in the deposition of a continental sedimentary column nearly 10000 m thick. There are different depositional sequences in these stages; the at composed mainly of volcanic rocks and alluvial fan—fan delta—lacustrine facies—swamp facies in the fault subsidence stage; mainly of alluvial plain-lacustrine facies in the fault downwarping stage; the mainly of alluvial plain—delta-extensive lacustrine facies in the downwarping stage; and that dominated by alluvial plain deposits with subordinate minor alluvial fan and relict lacustrine facies in the shrinkage stage. These constitute a composite depositional column fully displays the sedimentary characteristic of a failed continental rift basin, Facts indicate that two large-scale lake "invasions", synchronous with the global relative rise of sea level, which took place in the downwarping stage of the basin development, leading to the connection between lake and sea.
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