In lamina of shale which deposited in deep lake away from paleo-debouchment in the Shahejie Formation in the Jiyang Depression, some aeolian silty sand was discovered.
岩呈深灰色或棕褐色 ,理发育 ,主要由富含有机质纹层和浅灰色钙质纹层
的毫米级沉积层偶组。
In lamina of shale which deposited in deep lake away from paleo-debouchment in the Shahejie Formation in the Jiyang Depression, some aeolian silty sand was discovered.
岩呈深灰色或棕褐色 ,理发育 ,主要由富含有机质纹层和浅灰色钙质纹层的毫米级沉积层偶组。
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