黄土梁 meaning in Chinese
loess ridge
Examples
- The technique by facing huang - tu - liang reservoir with acrylic - emulsion cement mortar for preventing denudation of freezing - thaw is discussed in this paper
通过黄土梁水库进行工程护面处理，探讨了丙乳砂浆防止冻融剥蚀的应用技术，日后，可能得到较好效果的验证。 - But the conflict between them was appeared during our research in field and the discussion with others . it is followed that the former with the rolling bedrock , the mid with mild bedrock and the latter with the stable bedrock relatively . the conflict between two conclusion above arise , what relationship between loess landforms and their bedrock exist
但在野外调查及同其他学者交流中发现两者并非总体对应一致，显示出陕北黄土高原南部黄土塬基底起伏相对较大，北部黄土梁状(为主)丘陵沟壑区及黄土峁状(为主)丘陵沟壑区基底相对平坦的特征。 - According to the contractor on the case of the policemen , crime suspects in the lee case and the 51 - year - old man living in northwest guo baizhangzi pingquan county rural south huangtuliangzi village , li built before the highway came when diverted , and the opposite wei jia also because trees , piled straw diverted to the highway side of the river
据承办该案的公安干警介绍，犯罪嫌疑人李某与本案中的51岁的死者魏某都居住在平泉县郭杖子乡南黄土梁子村，李家以前修建院墙时挤占了公路，而对面的魏家也因栽树、堆放柴草挤占了公路边的河道。 - There is a evolutional phenomenon to have been recognized in shaanbei loess plateau from south to north . that is luochuan district with the loess yuan ( platform land ) in south . yan ' an - an ' sai district with the loess liang ( ridges ) mainly in middle and shunde - mizhi district with the loess mao ( rounded knolls ) mainly in north . this frame and tendency is got and thought to coincide with the styles of their bedrock traditionalh ? called conformability
在长期的研究和调查过程中，发现陕北黄土高原在南北纵向上存在明显的黄土地貌分异现象，即由南向北，大致依次为洛川黄土塬(广义)地貌、延安?安塞黄土梁状(为主)丘陵沟壑地貌、绥德?子洲黄土峁状(为主)沟壑地貌。 - The unconformability between the loess landform of shaanbei loess plateau and its bedrock shape was pointed out first after the full demonstration . the top of loess formation of the south part in shaanbei is flat which likes " platform " , the shape of the bedrock is rolling that likes ridge , and the bedrock bended to fold . the top of loess formation of the mid - part in shaanbei is rolling , but the shape of the bedrock below begins to get flat , the top of loess formation of the north part in shaanbei , loess mao district , is much more rolling among them , however , its shape of the bedrock below is the flattest relatively likes the platform shape of loess formation in south
具体地讲，陕北高原南部的洛） 11黄土源，黄上层顶部相对平坦，地貌类型以黄土源为主格调，而其下伏基岩地层诏皱相对发育，古地势起伏相对较大：陕北高原中部的延安一安塞黄土梁状（为主）丘陵沟壑区，黄土层顶部起伏相对增大，地貌类型以黄土梁为主格调，而其下伏基岩地层槽皱程度趋弱，地层较平缓，古地势起伏相对降低；陕北高原北部的绥德一子洲黄土赤状（为主）丘陵沟壑区，黄土层顶部起伏度相对最大，地貌类型以黄上赤为主格调，而其下伏基底地层以平缓为特征，古地势起伏强度亦相对较低。