1) Aeolian sand
风成砂
1.
And since then there are several aeolian sand units in loess.
9 Ma)以来粒度突然变粗并且地层中共发育了11层厚度较大的埋藏古风成砂,研究区远离沙漠,黄土中的砂粒及风成砂是近源搬运造成的,其中黄河河漫滩是其砂粒的主要供给源。
2) eolian sand
风成砂
1.
They also have diverse morphologies: erect tabular-flaky,vertical wedge-shaped, "⊥ "- and "U"-shaped,trapezoidal and dendritic forms, whichare usually filled by eolian sand and then turned into sandstone veins (dikes and.
形态多样，有直立板片状、直立楔状、“⊥”状、梯形状、“U”形状及树枝状等，其内有时被风成砂充填。
3) aeolian silty sand
风成粉砂
1.
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.
在济阳坳陷沙河街组远离古河口沉积的页岩纹层中发现了风成粉砂沉积。
4) eolian sandstone
风成砂岩
1.
Cretaceous eolian sandstones in the Kuqa basin on the northern margin of the Tarim basin: A case study of the Kuqa River section;
塔里木盆地北缘库车盆地白垩系风成砂岩研究——以库车河剖面为例
6) eolian placer
风成砂矿
补充资料：崩砂风
崩砂风
崩砂风 病名。见《喉科秘诀》卷下。参见大水风条。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条