A set of conglomerates of alluvial fan occurred in the second member of Yingcheng Formation of Liutai, southeast margin of Songliao Basin.
松辽盆地东南缘六台地区营城组二段发育一套冲积扇砾岩层。
A set of conglomerates of alluvial fan occurred in the second member of Yingcheng Formation of Liutai, southeast margin of Songliao Basin.
松辽盆地东南缘六台地区营城组二段发育一套冲积扇砾岩层。
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