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.
该油页岩呈深灰
褐 ,页理发育 ,主要由富含有机质纹层和浅灰钙质纹层
成的毫米级沉积层偶组成。
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.
该油页岩呈深灰褐 ,页理发育 ,主要由富含有机质纹层和浅灰钙质纹层成的毫米级沉积层偶组成。
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源自动生成，部分未经过人工审核，其表达内容亦不代表本软件的观点；若发现问题，欢迎向我们指正。
