1) buried sand ridges
埋藏沙脊
1.
The sand ridges on Stratum U14 which is bellow seafloor 90 m are buried sand ridges,and belong to TST(transgressive systems tract) of 320~200 ka BP,and the upper bounding surfaces of the sand ridge units are therefore considered as the MFS(maximum flooding surface) of this transgressive.
基于高分辨率的单道地震和多波束测深数据,识别并对比了东海陆架中部同一海区相距20余万年的层U14和层U2两期沙脊群,其中层U14期沙脊属于埋藏沙脊,位于东海海底以下90 m深处,推测属于距今320~200 ka的海侵体系域(TST),沙脊顶界面是该期海侵的最大洪泛面(MFS);层U2期沙脊位于东海陆架,属于衰退沙脊,系末次盛冰期(LGM)以来的TST,顶界面是LGM以来的MFS。
2) buried dune
埋藏沙丘
3) buried tidal sand bodies
埋藏潮沙体
4) buried soil under sand dunes
沙丘埋藏土壤
1.
It has been long held that the buried soil under sand dunes on the major sand lands in northern China formed due to the climatic changes of the Holocene, which could be used as a proxy record to reconstruct the past climate in warm-humid periods.
本文对我国东北沙地沙丘埋藏土壤的形成原因重新进行了探讨。
5) buried karst region
埋藏型岩溶垄脊槽谷区
1.
Karst hydrosystem is likely to suffer damage from human improper activities not only in bare karst region or cover karst region but also in buried karst region because of its natural fragility and susceptible character.
对比研究埋藏型岩溶垄脊槽谷区岩溶水质变化与土地利用的关系可以看出,研究区水质20年来的变化以及水质的空间变异与土地利用有很大的相关性;其中集约化的农业耕作、炸石填土增加土地面积、利用落水洞排放污水和独特的微型稻田水位控制设施对岩溶地下水水质产生显著影响;这也表明人类活动已经对该区水文地球化学产生了区域性的重大影响。
6) soil burying storage
埋藏
1.
At room temperature , effects of soil burying storage and garlic fresh-keeping agent treatment on Chinese yam were studied .
在室温条件下,研究了大蒜保鲜剂与埋藏处理对山药的贮藏效果。
2.
At room temperature,effects of soil burying storage treatment on Chinese yam were studied.
在室温条件下,研究了山药的埋藏保鲜方法。
补充资料：埋藏
1.掩埋尸体。 2.藏在泥土或其他细碎物体之中。 3.隐藏。
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